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  • Prairie blazing star (Liatris pycnostachya) also known as gayfeather is a common sight along the 1.5-mile Gayfeather Trail in the Regal Prairie Natural Area located in Prairie State Park. The park, located near Liberal, Mo. is Missouri’s largest remaining tallgrass prairie. The park’s nearly 4,000 acres is home to bison and elk. Panoramic hillsides of wildflowers such as prairie blazing star, sunflowers, and Indian paintbrush provide a canvas of color. In the fall, prairie grass such as big bluestem and Indian grass may tower as high as 8 feet tall. <br />
<br />
Tallgrass prairie once covered more than 13 million acres of Missouri’s landscape. Today, less than one percent remains. The prairie at Prairie State Park remains because the rocky land was too difficult to plow, which protected it from being farmed. Hiking, animal viewing, camping, birdwatching, and photography are some of the activities that the park affords. <br />
<br />
The Regal Prairie Natural Area is a 240-acre state natural area within the park that is especially noted for its wildflower display. The Nature Conservancy and the Missouri Prairie Foundation provided funding for the purchase of much of the park’s acreage. The area was dedicated as a state park in 1982.
    Prairie blazing star at sunset.jpg
  • Prairie blazing star (Liatris pycnostachya) also known as gayfeather is a common sight along the 1.5-mile Gayfeather Trail in the Regal Prairie Natural Area located in Prairie State Park. The park, located near Liberal, Mo. is Missouri’s largest remaining tallgrass prairie. The park’s nearly 4,000 acres is home to bison and elk. Panoramic hillsides of wildflowers such as prairie blazing star, sunflowers, and Indian paintbrush provide a canvas of color. In the fall, prairie grass such as big bluestem and Indian grass may tower as high as 8 feet tall. <br />
<br />
Tallgrass prairie once covered more than 13 million acres of Missouri’s landscape. Today, less than one percent remains. The prairie at Prairie State Park remains because the rocky land was too difficult to plow, which protected it from being farmed. Hiking, animal viewing, camping, birdwatching, and photography are some of the activities that the park affords. <br />
<br />
The Regal Prairie Natural Area is a 240-acre state natural area within the park that is especially noted for its wildflower display. The Nature Conservancy and the Missouri Prairie Foundation provided funding for the purchase of much of the park’s acreage. The area was dedicated as a state park in 1982.
    Prairie blazing star at sunset.jpg
  • Prairie blazing star (Liatris pycnostachya) also known as gayfeather is a common sight along the 1.5-mile Gayfeather Trail in the Regal Prairie Natural Area located in Prairie State Park. The park, located near Liberal, Mo. is Missouri’s largest remaining tallgrass prairie. The park’s nearly 4,000 acres is home to bison and elk. Panoramic hillsides of wildflowers such as prairie blazing star, sunflowers, and Indian paintbrush provide a canvas of color. In the fall, prairie grass such as big bluestem and Indian grass may tower as high as 8 feet tall. <br />
<br />
Tallgrass prairie once covered more than 13 million acres of Missouri’s landscape. Today, less than one percent remains. The prairie at Prairie State Park remains because the rocky land was too difficult to plow, which protected it from being farmed. Hiking, animal viewing, camping, birdwatching, and photography are some of the activities that the park affords. <br />
<br />
The Regal Prairie Natural Area is a 240-acre state natural area within the park that is especially noted for its wildflower display. The Nature Conservancy and the Missouri Prairie Foundation provided funding for the purchase of much of the park’s acreage. The area was dedicated as a state park in 1982.
    Prairie blazing star-4.jpg
  • Ashy sunflower (Helianthus mollis) grows along the 1.5-mile Gayfeather Trail in the Regal Prairie Natural Area located in Prairie State Park. The park, located near Liberal, Mo. is Missouri’s largest remaining tallgrass prairie. The park’s nearly 4,000 acres is home to bison and elk. Panoramic hillsides of wildflowers such as prairie blazing star, sunflowers, and Indian paintbrush provide a canvas of color. In the fall, prairie grass such as big bluestem and Indian grass may tower as high as 8 feet tall. <br />
<br />
Tallgrass prairie once covered more than 13 million acres of Missouri’s landscape. Today, less than one percent remains. The prairie at Prairie State Park remains because the rocky land was too difficult to plow, which protected it from being farmed. Hiking, animal viewing, camping, birdwatching, and photography are some of the activities that the park affords. <br />
<br />
The Regal Prairie Natural Area is a 240-acre state natural area within the park that is especially noted for its wildflower display. The Nature Conservancy and the Missouri Prairie Foundation provided funding for the purchase of much of the park’s acreage. The area was dedicated as a state park in 1982.
    Ashy sunflower on tallgrass prairie-...jpg
  • Death Valley National Park is a favorite for landscape photographers, particularly at sunrise and sunset. Here a photographer is silhouetted against the rising sun at the Mesquite Sand Dunes. The Mesquite Sand Dunes located in Death Valley National Park near Stovepipe Wells, is the largest dune field in the park. While the sand dunes appear tall, the highest dune only rises about 100 feet. The Mesquite Sand Dunes are the easiest sand dunes to visit in Death Valley National Park. Three types of dunes are found in the dune field: crescent, linear, and star shaped. The dune field is named for the Mesquite trees that create hummocks that provide places for wildlife to live.<br />
<br />
Death Valley National Park, located in eastern California near the border with Nevada is one of the hottest spots on earth, holding the hottest recorded air temperature of 134 °F. The Park also is location of the lowest spot in North America, 282 feet below sea level at the vast salt flats at Badwater Basin. At 3.4 million acres, the park is the largest national park in the contiguous United States. Death Valley National Park sits between the Panamint Range on the west  and Amargosa Range on the east.
    Silhouetted photographer at sunrise ...jpg
  • Death Valley National Park is a favorite for landscape photographers, particularly at sunrise and sunset. Here photographers are silhouetted against the rising sun at the Mesquite Sand Dunes. The Mesquite Sand Dunes located in Death Valley National Park near Stovepipe Wells, is the largest dune field in the park. While the sand dunes appear tall, the highest dune only rises about 100 feet. The Mesquite Sand Dunes are the easiest sand dunes to visit in Death Valley National Park. Three types of dunes are found in the dune field: crescent, linear, and star shaped. The dune field is named for the Mesquite trees that create hummocks that provide places for wildlife to live.<br />
<br />
Death Valley National Park, located in eastern California near the border with Nevada is one of the hottest spots on earth, holding the hottest recorded air temperature of 134 °F. The Park also is location of the lowest spot in North America, 282 feet below sea level at the vast salt flats at Badwater Basin. At 3.4 million acres, the park is the largest national park in the contiguous United States. Death Valley National Park sits between the Panamint Range on the west  and Amargosa Range on the east.
    Silhouetted photographers at sunrise...jpg
  • Death Valley National Park is a favorite for landscape photographers, particularly at sunrise and sunset. Here the sun rises in a blaze of color above the sand at the Mesquite Flat Sand Dunes. The Mesquite Flat Sand Dunes located in Death Valley National Park near Stovepipe Wells, is the largest dune field in the park. While the sand dunes appear tall, the highest dune only rises about 100 feet. The Mesquite Sand Dunes are the easiest sand dunes to visit in Death Valley National Park. Three types of dunes are found in the dune field: crescent, linear, and star shaped. The dune field is named for the Mesquite trees that create hummocks that provide places for wildlife to live.<br />
<br />
Death Valley National Park, located in eastern California near the border with Nevada is one of the hottest spots on earth, holding the hottest recorded air temperature of 134 °F. The Park also is location of the lowest spot in North America, 282 feet below sea level at the vast salt flats at Badwater Basin. At 3.4 million acres, the park is the largest national park in the contiguous United States. Death Valley National Park sits between the Panamint Range on the west  and Amargosa Range on the east.
    Mesquite Flat Sand Dunes sunrise.jpg
  • Bumblebees collect nectar and pollen from prairie blazing star (Liatris pycnostachya) also known as gayfeather along the 1.5-mile Gayfeather Trail in the Regal Prairie Natural Area located in Prairie State Park. The park, located near Liberal, Mo. is Missouri’s largest remaining tallgrass prairie. The park’s nearly 4,000 acres is home to bison and elk. Panoramic hillsides of wildflowers such as prairie blazing star, sunflowers, and Indian paintbrush provide a canvas of color. In the fall, prairie grass such as big bluestem and Indian grass may tower as high as 8 feet tall. <br />
<br />
Tallgrass prairie once covered more than 13 million acres of Missouri’s landscape. Today, less than one percent remains. The prairie at Prairie State Park remains because the rocky land was too difficult to plow, which protected it from being farmed. Hiking, animal viewing, camping, birdwatching, and photography are some of the activities that the park affords. <br />
<br />
The Regal Prairie Natural Area is a 240-acre state natural area within the park that is especially noted for its wildflower display. The Nature Conservancy and the Missouri Prairie Foundation provided funding for the purchase of much of the park’s acreage. The area was dedicated as a state park in 1982.
    Bumblebees and prairie blazing star-...jpg
  • Prairie blazing star (Liatris pycnostachya) also known as gayfeather is a common sight along the 1.5-mile Gayfeather Trail in the Regal Prairie Natural Area located in Prairie State Park. The park, located near Liberal, Mo. is Missouri’s largest remaining tallgrass prairie. The park’s nearly 4,000 acres is home to bison and elk. Panoramic hillsides of wildflowers such as prairie blazing star, sunflowers, and Indian paintbrush provide a canvas of color. In the fall, prairie grass such as big bluestem and Indian grass may tower as high as 8 feet tall. <br />
<br />
Tallgrass prairie once covered more than 13 million acres of Missouri’s landscape. Today, less than one percent remains. The prairie at Prairie State Park remains because the rocky land was too difficult to plow, which protected it from being farmed. Hiking, animal viewing, camping, birdwatching, and photography are some of the activities that the park affords. <br />
<br />
The Regal Prairie Natural Area is a 240-acre state natural area within the park that is especially noted for its wildflower display. The Nature Conservancy and the Missouri Prairie Foundation provided funding for the purchase of much of the park’s acreage. The area was dedicated as a state park in 1982.
    Prairie blazing star-5.jpg
  • Bumblebees collect nectar and pollen from prairie blazing star (Liatris pycnostachya) also known as gayfeather along the 1.5-mile Gayfeather Trail in the Regal Prairie Natural Area located in Prairie State Park. The park, located near Liberal, Mo. is Missouri’s largest remaining tallgrass prairie. The park’s nearly 4,000 acres is home to bison and elk. Panoramic hillsides of wildflowers such as prairie blazing star, sunflowers, and Indian paintbrush provide a canvas of color. In the fall, prairie grass such as big bluestem and Indian grass may tower as high as 8 feet tall. <br />
<br />
Tallgrass prairie once covered more than 13 million acres of Missouri’s landscape. Today, less than one percent remains. The prairie at Prairie State Park remains because the rocky land was too difficult to plow, which protected it from being farmed. Hiking, animal viewing, camping, birdwatching, and photography are some of the activities that the park affords. <br />
<br />
The Regal Prairie Natural Area is a 240-acre state natural area within the park that is especially noted for its wildflower display. The Nature Conservancy and the Missouri Prairie Foundation provided funding for the purchase of much of the park’s acreage. The area was dedicated as a state park in 1982.
    Bumblebees and prairie blazing star.jpg
  • Prairie blazing star (Liatris pycnostachya) also known as gayfeather is a common sight along the 1.5-mile Gayfeather Trail in the Regal Prairie Natural Area located in Prairie State Park. The park, located near Liberal, Mo. is Missouri’s largest remaining tallgrass prairie. The park’s nearly 4,000 acres is home to bison and elk. Panoramic hillsides of wildflowers such as prairie blazing star, sunflowers, and Indian paintbrush provide a canvas of color. In the fall, prairie grass such as big bluestem and Indian grass may tower as high as 8 feet tall. <br />
<br />
Tallgrass prairie once covered more than 13 million acres of Missouri’s landscape. Today, less than one percent remains. The prairie at Prairie State Park remains because the rocky land was too difficult to plow, which protected it from being farmed. Hiking, animal viewing, camping, birdwatching, and photography are some of the activities that the park affords. <br />
<br />
The Regal Prairie Natural Area is a 240-acre state natural area within the park that is especially noted for its wildflower display. The Nature Conservancy and the Missouri Prairie Foundation provided funding for the purchase of much of the park’s acreage. The area was dedicated as a state park in 1982.
    Prairie blazing star-3.jpg
  • Prairie blazing star (Liatris pycnostachya) also known as gayfeather is a common sight along the 1.5-mile Gayfeather Trail in the Regal Prairie Natural Area located in Prairie State Park. The park, located near Liberal, Mo. is Missouri’s largest remaining tallgrass prairie. The park’s nearly 4,000 acres is home to bison and elk. Panoramic hillsides of wildflowers such as prairie blazing star, sunflowers, and Indian paintbrush provide a canvas of color. In the fall, prairie grass such as big bluestem and Indian grass may tower as high as 8 feet tall. <br />
<br />
Tallgrass prairie once covered more than 13 million acres of Missouri’s landscape. Today, less than one percent remains. The prairie at Prairie State Park remains because the rocky land was too difficult to plow, which protected it from being farmed. Hiking, animal viewing, camping, birdwatching, and photography are some of the activities that the park affords. <br />
<br />
The Regal Prairie Natural Area is a 240-acre state natural area within the park that is especially noted for its wildflower display. The Nature Conservancy and the Missouri Prairie Foundation provided funding for the purchase of much of the park’s acreage. The area was dedicated as a state park in 1982.
    Prairie blazing star.jpg
  • Death Valley National Park is a favorite for landscape photographers, particularly at sunrise and sunset. Here the sun rises in a blaze of color above mountains as seen from the Mesquite Flat Sand Dunes.<br />
<br />
Death Valley National Park, located in eastern California near the border with Nevada is one of the hottest spots on earth, holding the hottest recorded air temperature of 134 °F. The Park also is location of the lowest spot in North America, 282 feet below sea level at the vast salt flats at Badwater Basin. At 3.4 million acres, the park is the largest national park in the contiguous United States. Death Valley National Park sits between the Panamint Range on the west  and Amargosa Range on the east.
    Death Valley sunrise.jpg
  • Prairie blazing star (Liatris pycnostachya) also known as gayfeather is a common sight along the 1.5-mile Gayfeather Trail in the Regal Prairie Natural Area located in Prairie State Park. The park, located near Liberal, Mo. is Missouri’s largest remaining tallgrass prairie. The park’s nearly 4,000 acres is home to bison and elk. Panoramic hillsides of wildflowers such as prairie blazing star, sunflowers, and Indian paintbrush provide a canvas of color. In the fall, prairie grass such as big bluestem and Indian grass may tower as high as 8 feet tall. <br />
<br />
Tallgrass prairie once covered more than 13 million acres of Missouri’s landscape. Today, less than one percent remains. The prairie at Prairie State Park remains because the rocky land was too difficult to plow, which protected it from being farmed. Hiking, animal viewing, camping, birdwatching, and photography are some of the activities that the park affords. <br />
<br />
The Regal Prairie Natural Area is a 240-acre state natural area within the park that is especially noted for its wildflower display. The Nature Conservancy and the Missouri Prairie Foundation provided funding for the purchase of much of the park’s acreage. The area was dedicated as a state park in 1982.
    Prairie blazing star-6.jpg
  • Prairie blazing star (Liatris pycnostachya) also known as gayfeather is a common sight along the 1.5-mile Gayfeather Trail in the Regal Prairie Natural Area located in Prairie State Park. The park, located near Liberal, Mo. is Missouri’s largest remaining tallgrass prairie. The park’s nearly 4,000 acres is home to bison and elk. Panoramic hillsides of wildflowers such as prairie blazing star, sunflowers, and Indian paintbrush provide a canvas of color. In the fall, prairie grass such as big bluestem and Indian grass may tower as high as 8 feet tall. <br />
<br />
Tallgrass prairie once covered more than 13 million acres of Missouri’s landscape. Today, less than one percent remains. The prairie at Prairie State Park remains because the rocky land was too difficult to plow, which protected it from being farmed. Hiking, animal viewing, camping, birdwatching, and photography are some of the activities that the park affords. <br />
<br />
The Regal Prairie Natural Area is a 240-acre state natural area within the park that is especially noted for its wildflower display. The Nature Conservancy and the Missouri Prairie Foundation provided funding for the purchase of much of the park’s acreage. The area was dedicated as a state park in 1982.
    Prairie blazing star-2.jpg
  • Ashy sunflower (Helianthus mollis) grows along the 1.5-mile Gayfeather Trail in the Regal Prairie Natural Area located in Prairie State Park. The park, located near Liberal, Mo. is Missouri’s largest remaining tallgrass prairie. The park’s nearly 4,000 acres is home to bison and elk. Panoramic hillsides of wildflowers such as prairie blazing star, sunflowers, and Indian paintbrush provide a canvas of color. In the fall, prairie grass such as big bluestem and Indian grass may tower as high as 8 feet tall. <br />
<br />
Tallgrass prairie once covered more than 13 million acres of Missouri’s landscape. Today, less than one percent remains. The prairie at Prairie State Park remains because the rocky land was too difficult to plow, which protected it from being farmed. Hiking, animal viewing, camping, birdwatching, and photography are some of the activities that the park affords. <br />
<br />
The Regal Prairie Natural Area is a 240-acre state natural area within the park that is especially noted for its wildflower display. The Nature Conservancy and the Missouri Prairie Foundation provided funding for the purchase of much of the park’s acreage. The area was dedicated as a state park in 1982.
    Ashy sunflower on tallgrass prairie.jpg
  • Fall colors are on display at Echo Bluff State Park in this view on the Painter Ridge Trail. In addition to hiking, the Painter Ridge Trail is also popular with mountain bikers with several mountain-bike-specific side trails containing curvy boardwalks and jumps. <br />
<br />
Sinking Creek which flows through Echo Bluff State Park is the second-largest tributary to the nearby Current River which is part of the Ozark National Scenic Riverways. <br />
<br />
Opening to the public in 2016 Echo Bluff is one of the state's newer parks. Echo Bluff State Park, located in Shannon County occupies the site of the former Camp Zoe. This summer camp for children operated for more than 85 years.<br />
<br />
Echo Bluff State Park is a popular hiking, mountain biking, floating, swimming, and fishing destination. A herd of wild horses can sometimes be seen in the area of the park. There are lodge rooms and full-service cabins available along with primitive to full-service campsites.
    Fall colors on Painter Ridge Trail.jpg
  • Rain approaches Avalanche Lake as seen from the Avalanche Lake Trail in Glacier National Park in Montana. Avalanche Lake was named in 1895 by a party including Dr. Lyman Sperry, namesake of the Sperry Glacier, who witnessed many avalanches during their stay. The meltwater from Sperry Glacier feeds the lake. Along the cliff face Monument Falls can be seen cascading down the mountain in the background. Avalanche Lake is the destination of the 4.5-mile roundtrip Avalanche Lake Trail.<br />
<br />
Glacier National Park in the Rocky Mountains of Montana encompasses more than 1 million acres. The park’s nickname is the “Crown of the Continent Ecosystem.” The park was established in May 1910. Soon after, hotels and chalets were established in the park, including the Lake McDonald Lodge. In 1932 construction began on the Going-to-the-Sun Road, allowing automobiles to traverse the park. Climate change is affecting the park. As of 2010, only 25 active glaciers remain in the park, down from the 150 that existed in the mid-19th century.
    Avalanche Lake.jpg
  • A fishing boat slowly makes its way through the fog in Auke Bay near Juneau, Alaska.
    Fishing boat in fog.jpg
  • The Saksaia Glacier sits at the top of the Glacier Creek valley near the location of the potential mine site being explored by Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan. The area of exploration, known as the Palmer Deposit is located near mile 40 of the Haines Highway and the Porcupine placer gold mining area near Haines, Alaska.<br />
<br />
The minerals that Constantine’s drilling explorations have found are primarily copper and zinc, with significant amounts of gold and silver. Exploratory drilling to refine the location and mineral amounts are the current focus of the company.<br />
<br />
If approved and developed, the mine would be an underground mine. Besides the actual ore deposits, having the nearby highway access for transporting ore to the deepwater port at Haines is also attractive to Constantine.<br />
<br />
Support for a large scale mine such as the Constantine project is divided among residents of Haines, a small community in Southeast Alaska 75 miles northwest of Juneau. The community’s needed economic boost from jobs, development and other mine support that a large-scale mine brings is tempting to some. To others, anything that might put the salmon spawning and rearing habitat and watershed resources at risk is simply unimaginable and unacceptable. Of particular concern is copper and other heavy metals in mine waste leaching into the Klehini and Chilkat River. Copper and heavy metals are toxic to salmon and bald eagles.<br />
<br />
The Chilkat River chum salmon are the primary food source for one of the largest gatherings of bald eagles in the world. Each fall, bald eagles congregate in the Alaska Chilkat Bald Eagle Preserve, located only three miles downriver from the area of current exploration. At times more than 3,000 eagles have been recorded at the primary gathering area for the fall chum salmon run.
    Saksaia Glacier 3.jpg
  • Eagle Glacier as seen from Favorite Channel just outside Juneau.
    Eagle Glacier-2.jpg
  • Rain approaches Avalanche Lake as seen from the Avalanche Lake Trail in Glacier National Park in Montana. Avalanche Lake was named in 1895 by a party including Dr. Lyman Sperry, namesake of the Sperry Glacier, who witnessed many avalanches during their stay. The meltwater from Sperry Glacier feeds the lake. Along the cliff face Monument Falls can be seen cascading down the mountain in the background. Avalanche Lake is the destination of the 4.5-mile roundtrip Avalanche Lake Trail.<br />
<br />
Glacier National Park in the Rocky Mountains of Montana encompasses more than 1 million acres. The park’s nickname is the “Crown of the Continent Ecosystem.” The park was established in May 1910. Soon after, hotels and chalets were established in the park, including the Lake McDonald Lodge. In 1932 construction began on the Going-to-the-Sun Road, allowing automobiles to traverse the park. Climate change is affecting the park. As of 2010, only 25 active glaciers remain in the park, down from the 150 that existed in the mid-19th century.<br />
<br />
EDITORS NOTE: The image is a composite panorama image.
    Avalanche Lake-2.jpg
  • Boulders from a landslide sprawl across a glacier that descends from Coleman Peak in Glacier Bay National Park and Preserve. This glacier eventually joins the McBride Glacier.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Landslide near Coleman Peak.jpg
  • A glacier descends from Coleman Peak in Glacier Bay National Park and Preserve to eventually join the McBride Glacier. Note the landslide in upper reaches of the glaicer.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Glacier near Coleman Peak.jpg
  • Glaciers flow from Mount Bertha (upper left) and Mount Crillon (upper right) to form the upper portion of Johns Hopkins Glacier in Glacier Bay National Park and Preserve.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Johns Hopkins Glacier.jpg
  • Two large glaciers come together to form the main flow of the McBride Glacier in Glacier Bay National Park and Preserve. The dark lines of rock debris are called medial moraines. A medial moraine is formed when two glaciers meet and the debris on the edges of the adjacent valley sides join and are carried on top of the glacier. <br />
<br />
The McBride Glacier, the most active glacier and only tidewater glacier in the Muir Inlet, is retreating.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Medial moraines, McBride Glacier.jpg
  • Fall colors and a scenic view of Mt. Emmerich greet visitors to Haines, Alaska. Haines is a cruise ship destination on the Lynn Canal in southeast Alaska. The Haines Highway provides road access to the continental highway system. The photograph was taken at Picture Point on AK-7 (Lutak Road).<br />
<br />
Haines, Alaska, a picturesque town in southeast Alaska, is located on the Lynn Canal between the towns of Skagway and Juneau. Haines is one of the few towns in southeast Alaska that is connected with the North American highway system. The Haines Highway (Alaska Route 7 or AK-7) travels through British Columbia and the Yukon (Yukon Highway 3) to connect with the Alaska Highway in Haines Junction, Yukon.<br />
<br />
Haines is also a stop on the Alaska Marine Highway System with ferries arriving from Skagway and Juneau.<br />
<br />
Wildlife viewing opportunities are abundant. The Alaska Chilkat Bald Eagle Preserve on the Chilkat River, near the confluence with the Tsirku River near Klukwan, is famous for its large concentration of bald eagles in the fall. At its peak in November, the American Bald Eagle Foundation sponsors the Alaska Bald Eagle Festival.
    Haines and Mt. Emmerich in fall.jpg
  • Clouds swirl around unnamed mountain peaks near Sinclair Mountain in the Kakuhan Range bask in this view seen from Picture Point in Haines, Alaska.
    Clouds and Kakuhan Range mountain pe...jpg
  • Fishing boats slowly make their way through the fog in Auke Bay near Juneau, Alaska.
    Fishing boats in fog.jpg
  • This aerial photograph of a portion of the "Council Grounds" is the primary area where bald eagles gather on the Chilkat River in the Alaska Chilkat Bald Eagle Preserve near Haines, Alaska. Bald eagles come to the alluvial delta area at the confluence of the Tsirku (center) and Chilkat (upper left to right) Rivers because of the availability of spawned-out salmon and open waters in late fall and early winter. The open water is due to a deep accumulation of gravel and sand that acts as a large water reservoir whose water temperature remains 10 to 20 degrees warmer than the surrounding water temperature. This warmer water seeps into the Chilkat River, keeping a five mile stretch of the river from freezing. Photographers come to the Chilkat River in November and December to photograph one of the largest gatherings of bald eagles in the world. In 1982, the 48,000 acre area was designated as the Alaska Chilkat Bald Eagle Preserve. In the background are the mountains that make of the Takshanuk Mountains. Chilkat Lake is pictured in the foreground. River on the left above the Tsirku River is the Klehini River which joins the Chilkat River right before the Tsirku River alluvial fan. Also pictured is Klutshah Mountain (top center), Iron Mountain and the village of Klukwan (in front of the left side of the alluvial fan).
    Tsirku River alluvial fan with Chilk...jpg
  • The conflict over putting in a hard-rock mine near the Alaska Chilkat Bald Eagle Preserve near Haines, Alaska took a new turn recently with the filing of a lawsuit by an Alaska Native Tlingit tribe and three environmental groups. The group is suing the Bureau of Land Management, saying that the agency granted mineral exploration permits without considering how a mine could affect the Chilkat River's salmon and the Alaska Chilkat Bald Eagle Preserve.<br />
<br />
Constantine Metal Resources and investment partner Dowa Metals & Mining Co., Ltd. of Japan are exploring a potential site for a mine on the steep mountain slopes pictured above Glacier Creek. This area is known as the Palmer Deposit.<br />
<br />
Joining the Tlingit village of Klukwan in the lawsuit against the Bureau of Land Management are the Southeast Alaska Conservation Council, Lynn Canal Conservation and Rivers Without Borders. They are represented by Earthjustice, a nonprofit environmental law firm. The group is asking for mining permits to be revoked.<br />
<br />
In August 2015, Constantine Metal Resources Ltd. of Vancouver, British Columbia submitted a plan with the BLM to extend their existing access road by 2.5 miles including a switchback road leading to a staging area at the 800 ft. level on the side of the 1,700 ft. mountainside. A proposed bridge crossing Glacier Creek would be located in the shadow area in the lower center of the photo with a switchback road leading from the Glacier Creek to the staging area for helicopter and ground-supported activities on the left. The road would also provide access for up to 40 new exploration drill sites. Pictured in the background is the Klehini River. A map showing exactly how this road would appear can be found here: https://eplanning.blm.gov/epl-front-office/projects/nepa/54990/65845/71485/Figure_6.4_accessible.pdf<br />
<br />
The group suing is concerned that copper and other heavy metals in mine waste might leech into the nearby Klehini River and the Chilkat River, 14 miles downstream.
    Constantine Palmer Deposit aerial -2.jpg
  • The conflict over putting in a hard-rock mine near the Alaska Chilkat Bald Eagle Preserve near Haines, Alaska took a new turn recently with the filing of a lawsuit by an Alaska Native Tlingit tribe and three environmental groups. The group is suing the Bureau of Land Management, saying that the agency granted mineral exploration permits without considering how a mine could affect the Chilkat River's salmon and the Alaska Chilkat Bald Eagle Preserve. <br />
<br />
Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan is exploring a potential site for a mine (located on the upper left side of image) just above Glacier Creek (foreground) and the Klehini River (right side of image). The border with British Columbia is at the upper right. The area above Glacier Greek, known as the Palmer Deposit is located near mile 40 of the Haines Highway.<br />
<br />
The minerals that Constantine’s drilling explorations have found are primarily copper and zinc, with significant amounts of gold and silver.<br />
<br />
Support for a large scale mine such as the Constantine project is divided among residents of Haines, a small community in Southeast Alaska 75 miles northwest of Juneau. The community’s needed economic boost from jobs, development and other mine support that a large-scale mine brings is tempting to some. To others, anything that might put the salmon spawning and rearing habitat and watershed resources at risk is simply unimaginable and unacceptable. Of particular concern is copper and other heavy metals in mine waste leaching into the Klehini River (shown) and the Chilkat River 14 miles downstream. Copper and heavy metals are toxic to salmon and bald eagles.<br />
<br />
The Chilkat River chum salmon are the primary food source for one of the largest gatherings of bald eagles in the world. Each fall, bald eagles congregate in the Alaska Chilkat Bald Eagle Preserve, located only three miles downriver from the area of current exploration
    Constantine Palmer Deposit aerial.jpg
  • A spectacular display of the Aurora Borealis or as it is commonly called, the northern lights, occurred the evening of November 8 through the early morning of November 9, 2013 over Sinclair Mountain and other mountains in the Kakuhan Range at Haines, Alaska. The luminous glow in the upper atmosphere stretched across the skies above the Lynn Canal from Skagway to Juneau. The bottom edge of an aurora is typically 60 miles high with the top edge at an altitude of 120 to 200 miles, though sometimes high altitude aurora can be as high as 350 miles. The collision of sun storm electrons and protons with different types of gas particles in Earth’s atmosphere cause the different colors. Green, the most common color, is caused by the collision of electrons with atoms of with atomic oxygen.
    Aurora Borealis over Haines, Alaska-...jpg
  • Moss covers the forest floor along the Trail of Time Trail near the Mendenhall Lake and Mendhenall Visitor Center just outside Juneau, Alaska.
    Moss along Trail of Time Trail.jpg
  • Mount Golub, a 4194 foot peak in the Chilkat Range as seen from the Favorite Channel near Juneau, Alaska.
    Mount Golub.jpg
  • Common horsetail (Equisetum arvense) along the Chilkoot Indian Association Trail in Haines, Alaska. Common horsetail is a fern. Moose, caribou, sheep and bears eat this plant.
    Common horsetail.jpg
  • Panorama of Haines, Alaska townsite area (center), including the Lynn Canal (right), Mount Villard (right). Mount Ripinski (center) and the Chilkat River (left). EDITOR’S NOTE: The image is a panoramic composite made up of several overlapping images.
    Haines, Lynn Canal panorama.jpg
  • The main bay of Glacier Bay National Park and Preserve is vast, stretching 69 miles from its mouth to the furthest extent. It is hard to imagine that the area pictured (a small portion of the bay) was a single large glacier of solid ice only a little over 200 years ago. In the mid-1700s, this view (and quite a bit beyond) would have been covered by a glacier nearly a mile in thickness. Since then, the massive glacier that filled the bay has retreated 69 miles to the heads of various inlets. <br />
<br />
Recent research determined that there is 11% less glacial ice in Glacier Bay  than in the 1950s. Still, even with the earth’s rapidly changing climate, Glacier Bay is home to a few stable glaciers due to heavy snowfall in the nearby Fairweather Mountains. <br />
<br />
The pictured view is of the Beartrack Mountains looking from Tlingit Point on the left to North Marble Island and South Marble Island on the far right.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. The park is also an important marine wilderness area known for its spectacular tidewater glaciers, icefields, and tall coastal mountains. The park, a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales, which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, Steller sea lions, and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.<br />
<br />
EDITOR’S NOTE: The image is a panoramic composite of several overlapping images.
    Beartrack Mountains panorama.jpg
  • Fall colors are on display at Echo Bluff State Park in this view on the Painter Ridge Trail. In addition to hiking, the Painter Ridge Trail is also popular with mountain bikers with several mountain-bike-specific side trails containing curvy boardwalks and jumps. <br />
<br />
Sinking Creek which flows through Echo Bluff State Park is the second-largest tributary to the nearby Current River which is part of the Ozark National Scenic Riverways. <br />
<br />
Opening to the public in 2016 Echo Bluff is one of the state's newer parks. Echo Bluff State Park, located in Shannon County occupies the site of the former Camp Zoe. This summer camp for children operated for more than 85 years.<br />
<br />
Echo Bluff State Park is a popular hiking, mountain biking, floating, swimming, and fishing destination. A herd of wild horses can sometimes be seen in the area of the park. There are lodge rooms and full-service cabins available along with primitive to full-service campsites.
    Fall colors on Painter Ridge Trail-2.jpg
  • Christmas ferns poke through the forest leaf litter in Echo Bluff State Park on the Painter Ridge Trail. Christmas fern (Polystichum acrostichoides) is one of the most common ferns in Missouri forests. Its leaves are evergreen, and pioneers used it for making Christmas wreaths.<br />
<br />
In addition to hiking, the Painter Ridge Trail is also popular with mountain bikers with several mountain-bike-specific side trails containing curvy boardwalks and jumps. <br />
<br />
Sinking Creek which flows through Echo Bluff State Park is the second-largest tributary to the nearby Current River which is part of the Ozark National Scenic Riverways. <br />
<br />
Opening to the public in 2016 Echo Bluff is one of the state's newer parks. Echo Bluff State Park, located in Shannon County occupies the site of the former Camp Zoe. This summer camp for children operated for more than 85 years.<br />
<br />
Echo Bluff State Park is a popular hiking, mountain biking, floating, swimming, and fishing destination. A herd of wild horses can sometimes be seen in the area of the park. There are lodge rooms and full-service cabins available along with primitive to full-service campsites.
    Christmas fern.jpg
  • Fall colors are on display at Echo Bluff State Park in this view from the Painter Ridge Trail near the Bluff Top Pavilion. In addition to hiking, the Painter Ridge Trail is also popular with mountain bikers with several mountain-bike-specific side trails containing curvy boardwalks and jumps. <br />
<br />
Sinking Creek which flows through Echo Bluff State Park is the second-largest tributary to the nearby Current River which is part of the Ozark National Scenic Riverways. <br />
<br />
Opening to the public in 2016 Echo Bluff is one of the state's newer parks. Echo Bluff State Park, located in Shannon County occupies the site of the former Camp Zoe. This summer camp for children operated for more than 85 years.<br />
<br />
Echo Bluff State Park is a popular hiking, mountain biking, floating, swimming, and fishing destination. A herd of wild horses can sometimes be seen in the area of the park. There are lodge rooms and full-service cabins available along with primitive to full-service campsites.
    Fall leaves.jpg
  • Fall colors are on display at Echo Bluff State Park in this view from the Painter Ridge Trail near the Bluff Top Pavilion. The park’s namesake, Echo Bluff (upper right) overlooks Sinking Creek. Sinking Creek which flows through Echo Bluff State Park is the second-largest tributary to the nearby Current River which is part of the Ozark National Scenic Riverways. <br />
<br />
In addition to hiking, the Painter Ridge Trail is also popular with mountain bikers with several mountain-bike-specific side trails containing curvy boardwalks and jumps. <br />
<br />
Opening to the public in 2016 Echo Bluff is one of the state's newer parks. Echo Bluff State Park, located in Shannon County occupies the site of the former Camp Zoe. This summer camp for children operated for more than 85 years.<br />
<br />
Echo Bluff State Park is a popular hiking, mountain biking, floating, swimming, and fishing destination. A herd of wild horses can sometimes be seen in the area of the park. There are lodge rooms and full-service cabins available along with primitive to full-service campsites.
    Echo Bluff and Sinking Creek-2.jpg
  • Lake McDonald is the largest of the glacially carved lakes in Glacier National Park in Montana. Lake McDonald is ten miles long and 472 feet deep. While the lake has numerous species of fish, the fishing is considered poor due to the lack of nutrients in the lake.  Western red cedar and hemlock are found in the lake’s valley.<br />
<br />
Glacier National Park in the Rocky Mountains of Montana encompasses more than 1 million acres. The park’s nickname is the “Crown of the Continent Ecosystem.” The park was established in May 1910. Soon after, hotels and chalets were established in the park, including the Lake McDonald Lodge. In 1932 construction began on the Going-to-the-Sun Road, allowing automobiles to traverse the park. Climate change is affecting the park. As of 2010, only 25 active glaciers remain in the park, down from the 150 that existed in the mid-19th century.
    Lake McDonald.jpg
  • A spectacular display of the Aurora Borealis or as it is commonly called, the northern lights, occurred the evening of November 8 through the early morning of November 9, 2013 over Sinclair Mountain and other mountains in the Kakuhan Range at Haines, Alaska. The luminous glow in the upper atmosphere stretched across the skies above the Lynn Canal from Skagway to Juneau. The bottom edge of an aurora is typically 60 miles high with the top edge at an altitude of 120 to 200 miles, though sometimes high altitude aurora can be as high as 350 miles. The collision of sun storm electrons and protons with different types of gas particles in Earth’s atmosphere cause the different colors. Green, the most common color, is caused by the collision of electrons with atoms of with atomic oxygen. *** EDITORS NOTE: Blue rocks are result of use of tungsten white balance at time of image capture. Boulders in foreground were lit with a flashlight during time exposure***
    Aurora Borealis over Haines, Alaska-...jpg
  • A meadow of tall fireweed booms in Brotherhood Bridge Park in Juneau, Alaska. In the background is the Mendenhall Glacier, one of the most accessible glaciers in southeast Alaska. Each year, 465,000 curise ship passengers visit the Mendenhall Glacier.
    Tall fireweed and Mendenhall Glacier.jpg
  • Mount Crillon (12,726 ft.) rises above the clouds near the Johns Hopkins Glacier in Glacier in Glacier Bay National Park and Preserve.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Mount Crillion.jpg
  • The shadow of a small plane passes over the border of Glacier Bay National Park and Preserve above uppermost reaches of McBride Glacier near Mount Krause.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Upper McBride Glacier.jpg
  • This aerial view shows the last portion of the McBride Glacier before it meets the ocean in Glacier Bay National Park and Preserve. The McBride Glacier is the most active glacier and only tidewater glacier in the Muir Inlet, is retreating. Muir Inlet can be seen in the upper right of the photo.<br />
<br />
The dark line of rock debris is called called a medial moraine. A medial moraine is formed when two glaciers meet and the debris on the edges of the adjacent valley sides join and are carried on top of the glacier.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Medial moraine, McBride Glacier.jpg
  • The steep valley wall of the Tsirku River near Haines, Alaska were made by the Tsirku Glacier. This photo was taken near the U.S. and Canadian border, near the terminus of the glacier.
    Tsirku River valley wall.jpg
  • The gravel bars of the braided Chilkat River take on the form of a bird in done in northwestern coast art style.
    Chilkat River gravel bar art.jpg
  • The 19-mile long Fairweather Glacier flows past the Lituya Mountain (left) in Glacier Bay National Park and Preserve.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Fairweather Glacier.jpg
  • Deep crevasses of Margerie Glacier take on an other worldly look in early evening light in this photo taken at the uppermost region of the glacier just inside the U.S. at the Canadian border. The 21-mile-long glacier in Glacier Bay National Park and Preserve is one of the park’s tidewater glaciers. <br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Margerie Glacier crevasses-2.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Alaska Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
Mountainsides that were held strong by the heavy ice of glaciers become weak when the glaciers retreat. Erosion along with earthquakes are triggers that can cause the weakened slopes to collapse.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide-9.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Anchorage Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
This aerial photo of the Lamplugh Glacier landslide was taken two days after the landslide.
    Lamplugh Glacier landslide-8.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Anchorage Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide-5.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Anchorage Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide-3.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Anchorage Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide.jpg
  • Unknown trees near the end of the Glacier Highway north of Juneau.
    Trees near end of Lynn Canal highway...jpg
  • The Milky Way stretches across the sky above the peaks of Mt. Emmerich and the Takhinsha Mountains in this photo taken along the Chilkat River near Haines, Alaska .
    Milky Way over Mt. Emmerich.jpg
  • The Milky Way stretches across the sky above Haines, Alaska and the Chilkat Mountains in this photo taken at Picture Point.
    Milky way over Haines.jpg
  • A lone fisherman fishes at the outlet of Chilkoot Lake at the Chilkoot Lake State Recreation Site near Haines, Alaska. <br />
<br />
The Chilkoot River outlet of Chilkoot Lake offers some of the best salmon fishing in Southeast Alaska. Four salmon runs are an open invitation for bears to feast on the spawning salmon. At times, the Chilkoot River Corridor has some of the highest bear activity in the state. The Chilkoot River corridor area is extremely narrow with room for an equally narrow road with few pullouts for tourists and fisherman causing traffic and congestion. This creates a serious conflict between humans and bears.<br />
<br />
The Chilkoot River ranks second in popularity for Southeast Alaska freshwater sports fishing. The area is also an important cultural area for the Tlingit people and site of a culture camp.
    Lone fisherman fiishing on Chilkoot ...jpg
  • The conflict over putting in a hard-rock mine near the Alaska Chilkat Bald Eagle Preserve near Haines, Alaska took a new turn recently with the filing of a lawsuit by an Alaska Native Tlingit tribe and three environmental groups. The group is suing the Bureau of Land Management, saying that the agency granted mineral exploration permits without considering how a mine could affect the Chilkat River's salmon and the Alaska Chilkat Bald Eagle Preserve. <br />
<br />
Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan is exploring a potential site for a mine (located on the upper left side of image) just above Glacier Creek (foreground) and the Klehini River (right side of image). The border with British Columbia is at the upper right. The area above Glacier Greek, known as the Palmer Deposit is located near mile 40 of the Haines Highway.<br />
<br />
The minerals that Constantine’s drilling explorations have found are primarily copper and zinc, with significant amounts of gold and silver.<br />
<br />
Support for a large scale mine such as the Constantine project is divided among residents of Haines, a small community in Southeast Alaska 75 miles northwest of Juneau. The community’s needed economic boost from jobs, development and other mine support that a large-scale mine brings is tempting to some. To others, anything that might put the salmon spawning and rearing habitat and watershed resources at risk is simply unimaginable and unacceptable. Of particular concern is copper and other heavy metals in mine waste leaching into the Klehini River (shown) and the Chilkat River 14 miles downstream. Copper and heavy metals are toxic to salmon and bald eagles.<br />
<br />
The Chilkat River chum salmon are the primary food source for one of the largest gatherings of bald eagles in the world. Each fall, bald eagles congregate in the Alaska Chilkat Bald Eagle Preserve, located only three miles downriver from the area of current exploration
    Constantine Palmer Deposit aerial -7.jpg
  • Aerial photo of the Chilkat Peninsula (left to right center) and the McClellan Flats area of the Chilkat River where the river meets the Lynn Canal. Also pictured is Pyramid Island (the tiny island (center), the Kakuhan Range (tallest mountains in background) and Mt. Riley (left) that is part of the Chilkat Peninsula.
    Low sun on Chilkat Inlet,.jpg
  • The conflict over putting in a hard-rock mine near the Alaska Chilkat Bald Eagle Preserve near Haines, Alaska took a new turn recently with the filing of a lawsuit by an Alaska Native Tlingit tribe and three environmental groups. The group is suing the Bureau of Land Management, saying that the agency granted mineral exploration permits without considering how a mine could affect the Chilkat River's salmon and the Alaska Chilkat Bald Eagle Preserve. <br />
<br />
Joining the Tlingit village of Klukwan in the lawsuit against the Bureau of Land Management are the Southeast Alaska Conservation Council, Lynn Canal Conservation and Rivers Without Borders. They are represented by Earthjustice, a nonprofit environmental law firm. The group is asking for mining permits to be revoked.<br />
<br />
Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan is exploring a potential site, known as the Palmer Deposit for a mine (located upper center right) just above Glacier Creek (not visible) and the Klehini River (foreground). Pictured in the rear of the photo is Saksaia Glacier.<br />
<br />
Support for a large scale mine is divided among residents of Haines. The community’s needed economic boost from jobs that a large-scale mine brings is tempting to some. To others, anything that might put the salmon spawning and rearing habitat and watershed resources at risk is simply unimaginable and unacceptable. Of particular concern is copper and other heavy metals in mine waste leaching into the Klehini River (shown) and the Chilkat River 14 miles downstream. Copper and heavy metals are toxic to salmon and bald eagles.<br />
<br />
The Chilkat River chum salmon are the primary food source for one of the largest gatherings of bald eagles in the world. Each fall, bald eagles congregate in the Alaska Chilkat Bald Eagle Preserve, located only three miles downriver from the area of current exploration.
    Constantine Mine 2, Palmer Deposit.jpg
  • The conflict over putting in a hard-rock mine near the Alaska Chilkat Bald Eagle Preserve near Haines, Alaska took a new turn recently with the filing of a lawsuit by an Alaska Native Tlingit tribe and three environmental groups. The group is suing the Bureau of Land Management, saying that the agency granted mineral exploration permits without considering how a mine could affect the Chilkat River's salmon and the Alaska Chilkat Bald Eagle Preserve. <br />
<br />
Joining the Tlingit village of Klukwan in the lawsuit against the BLM are the Southeast Alaska Conservation Council, Lynn Canal Conservation and Rivers Without Borders. They are represented by Earthjustice, a nonprofit environmental law firm. The group is asking for mining permits to be revoked.<br />
<br />
Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan is exploring a site for a mine located just to the right of the pictured Saksaia Glacier (right). The potential mine site is just above Glacier Creek (not visible) and the Klehini River (foreground). This area, known as the Palmer Deposit, is located near the Porcupine placer gold mining area (the low foreground area) below Porcupine Peak (left rear).<br />
<br />
Support for a large scale mine is divided among area residents. The needed economic boost from jobs that a mine brings is tempting to some. To others, anything that might put the salmon spawning and rearing habitat and watershed resources at risk is simply unimaginable and unacceptable. The concern is copper and other heavy metals in mine waste leaching into the Klehini River (shown) and the Chilkat River 14 miles downstream.<br />
<br />
The Chilkat River salmon are the primary food source for one of the largest gatherings of bald eagles in the world. Each fall, bald eagles congregate in the Alaska Chilkat Bald Eagle Preserve located only three miles downriver from the area of current exploration.<br />
<br />
EDITORS NOTE: This image is a stitched panorama.
    Porcupine - Constantine Palmer Depos...jpg
  • A spectacular display of the Aurora Borealis or as it is commonly called, the northern lights, occurred the evening of November 8 through the early morning of November 9, 2013 over Haines, Alaska. The luminous glow in the upper atmosphere stretched across the skies above the Lynn Canal from Skagway to Juneau. The bottom edge of an aurora is typically 60 miles high with the top edge at an altitude of 120 to 200 miles, though sometimes high altitude aurora can be as high as 350 miles. The collision of sun storm electrons and protons with different types of gas particles in Earth’s atmosphere cause the different colors. Green, the most common color, is caused by the collision of electrons with atoms of with atomic oxygen.
    Aurora Borealis over Haines, Alaska.jpg
  • Aerial view of Knight Inlet seen from an Alaska Airlines flight to Juneau. Knight Inlet is one of the main inlets of British Columbia. At 79 miles, is one of the longest on the British Columbia coast. It is known for the severe turbulence at its mouth during tide changes for the outflow winds that flow from the interior mountains. Glacier Peak and Mount Kennedy can be seen in the center left of the photo.
    Knight Inlet,.jpg
  • Davidson Glacier is framed by Talsani Island and the tip of the Chilkat Peninsula, in this view from the Lynn Canal near Haines, Alaska.
    Davidson Glacier.jpg
  • A acorn barnacle and rockweed-covered boulder on the shore of the Muir Inlet of the East Arm of Glacier Bay National Park and Preserve in Alaska. Red Mountain is the mountain in the left-center of the photo.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. The park is also an important marine wilderness area known for its spectacular tidewater glaciers, icefields, and tall coastal mountains. The park, a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions, and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Muri Inlet.jpg
  • The Sun sets over Eider and Strawberry Islands, located in the Beardslee Islands in Glacier Bay National Park and Preserve.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. The park is also an important marine wilderness area known for its spectacular tidewater glaciers, icefields, and tall coastal mountains. The park, a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions, and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Beardslee Islands sunset.jpg
  • Lion Lake, a popular recreation area, near Hungry Horse, Montana is located in the Flathead National Forest. The U.S. Bureau of Reclamation dammed the lake in the late 1940s to supply water for a government work camp during the construction of the larger Hungry Horse Dam.
    Lion Lake.jpg
  • This view of the gorge of Avalanche Creek is from the Trail of the Cedars, a wheelchair-accessible loop trail, that begins and ends along the Going-to-the-Sun Road in Glacier National Park in Montana. The 4.5 mile roundtrip hike to Avalanche Lake begins near here.<br />
<br />
Glacier National Park in the Rocky Mountains of Montana encompasses more than 1 million acres. The park’s nickname is the “Crown of the Continent Ecosystem.” The park was established in May 1910. Soon after, hotels and chalets were established in the park, including the Lake McDonald Lodge. In 1932 construction began on the Going-to-the-Sun Road, allowing automobiles to traverse the park. Climate change is affecting the park. As of 2010, only 25 active glaciers remain in the park, down from the 150 that existed in the mid-19th century.
    Avalanche Creek.jpg
  • Glaciers flow  into the Wachusett Inlet of the East Arm of Glacier Bay National Park and Preserve.  Peak at upper left is Mount Merriam. In the very distant upper right Mount Bertha, located in the Fairweather Range, can be seen.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Mount Merriam.jpg
  • The Tsirku River is a braided river near Haines, Alaska that eventually flows into the Chilkat River. At that intersection of the two rivers, the Tsirku River spreads out into a huge alluvial fan river delta. That area, is the primary area where bald eagles gather on the Chilkat River in the Alaska Chilkat Bald Eagle Preserve. This downriver view of the Tsirku River is several miles before the river leaves the steep walls of the river valley and forms the alluvial fan river delta.<br />
<br />
Bald eagles come to the alluvial delta area at the confluence of the Tsirku and Chilkat Rivers because of the availability of spawned-out salmon and open waters in late fall and early winter. The open water is due to a deep accumulation of gravel and sand that acts as a large water reservoir whose water temperature remains 10 to 20 degrees warmer than the surrounding water temperature. This warmer water seeps into the Chilkat River, keeping a five mile stretch of the river from freezing.
    Tsirku River.jpg
  • Cracks in the snow on the mountainside above the Fairweather Glacier appear like they could cause an avalanche in Glacier Bay National Park and Preserve.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Fairweather Glacier snow cracks.jpg
  • Gray silted water flows from an alluvial fan into the clear blue ocean of the Queen Inlet in the West Arm of Glacier Bay National Park and Preserve. Silt and debris formed the the alluvial fan from the melting water of a glacier near Mount Merriam. <br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Glacier alluvial fan.jpg
  • Little remains of the Burroughs Glacier (center). In the foreground, are the snow-covered tops of Minnesota Ridge. On the other side of Burroughs Glacier are the Bruce Hills, followed by Wachusett Inlet. The far side of the inlet are the mountains of Idaho Ridge including: Mount Kloh Kutz, Mount Cadell, Mount Merriam and Mount Wordie. In the very distant upper part of the image, mountains of the Fairweather Range can be seen.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Burroughs Glacier.jpg
  • Fireweed (Chamaenerion angustifolium) blooms across from islands in the Lynn Canal. In the background are the mountains of the Chilkat Range. This view is from a pullout on the Glacier Highway, north of Juneau.
    Fireweed,.jpg
  • Deep crevasses of Margerie Glacier take on an other worldly look in early evening light in this photo taken at the uppermost region of the glacier just inside the U.S. at the Canadian border. The 21-mile-long glacier in Glacier Bay National Park and Preserve is one of the park’s tidewater glaciers. <br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Margerie Glacier crevasses.jpg
  • Fallen debris on the side of a valley of the Johns Hopkins Glacier in Glacier Bay National Park and Preserve appears to be almost feather-like.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Johns Hopkins Glacier debris.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Anchorage Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
This aerial photo of the Lamplugh Glacier landslide was taken two days after the landslide.
    Lamplugh Glacier landslide-7.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Alaska Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
Mountainsides that were held strong by the heavy ice of glaciers become weak when the glaciers retreat. Erosion along with earthquakes are triggers that can cause the weakened slopes to collapse.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide-6.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Alaska Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
Mountainsides that were held strong by the heavy ice of glaciers become weak when the glaciers retreat. Erosion along with earthquakes are triggers that can cause the weakened slopes to collapse.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide-4.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Alaska Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
Mountainsides that were held strong by the heavy ice of glaciers become weak when the glaciers retreat. Erosion along with earthquakes are triggers that can cause the weakened slopes to collapse.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide-2.jpg
  • The mountains of the Kakuhan Range in the Tongass National Forest can be seen in the view from Mud Bay near Haines, Alaska on the Lynn Canal. EDITORS NOTE: Image is a panoramic composite of multiple overlapping images.
    Mud Bay view panorama.jpg
  • The mountains of the Kakuhan Range in the Tongass National Forest can be seen in the view from Mud Bay near Haines, Alaska on the Lynn Canal.
    Mud Bay view, Haines.jpg
  • Aspen trees show off their fall colors along Herman Creek near Haines, Alaska.
    Aspen trees along Herman Creek.jpg
  • The Saksaia Glacier sits at the top of the Glacier Creek valley near the location of the potential mine site being explored by Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan. The area of exploration, known as the Palmer Deposit is located near mile 40 of the Haines Highway and the Porcupine placer gold mining area near Haines, Alaska.<br />
<br />
The minerals that Constantine’s drilling explorations have found are primarily copper and zinc, with significant amounts of gold and silver. Exploratory drilling to refine the location and mineral amounts are the current focus of the company.<br />
<br />
If approved and developed, the mine would be an underground mine. Besides the actual ore deposits, having the nearby highway access for transporting ore to the deepwater port at Haines is also attractive to Constantine.<br />
<br />
Support for a large scale mine such as the Constantine project is divided among residents of Haines, a small community in Southeast Alaska 75 miles northwest of Juneau. The community’s needed economic boost from jobs, development and other mine support that a large-scale mine brings is tempting to some. To others, anything that might put the salmon spawning and rearing habitat and watershed resources at risk is simply unimaginable and unacceptable. Of particular concern is copper and other heavy metals in mine waste leaching into the Klehini and Chilkat River. Copper and heavy metals are toxic to salmon and bald eagles.<br />
<br />
The Chilkat River chum salmon are the primary food source for one of the largest gatherings of bald eagles in the world. Each fall, bald eagles congregate in the Alaska Chilkat Bald Eagle Preserve, located only three miles downriver from the area of current exploration. At times more than 3,000 eagles have been recorded at the primary gathering area for the fall chum salmon run.
    Saksaia Glacier 1.jpg
  • The conflict over putting in a hard-rock mine near the Alaska Chilkat Bald Eagle Preserve near Haines, Alaska took a new turn recently with the filing of a lawsuit by an Alaska Native Tlingit tribe and three environmental groups. The group is suing the Bureau of Land Management, saying that the agency granted mineral exploration permits without considering how a mine could affect the Chilkat River's salmon and the Alaska Chilkat Bald Eagle Preserve. <br />
<br />
Joining the Tlingit village of Klukwan in the lawsuit against the Bureau of Land Management are the Southeast Alaska Conservation Council, Lynn Canal Conservation and Rivers Without Borders. They are represented by Earthjustice, a nonprofit environmental law firm. The group is asking for mining permits to be revoked.<br />
<br />
Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan is exploring a potential site for a mine, known as the Palmer Deposit, (located upper right) just above Glacier Creek (not visible) and the Klehini River (foreground).<br />
<br />
Support for a large scale mine is divided among residents of Haines. The community’s needed economic boost from jobs that a large-scale mine brings is tempting to some. To others, anything that might put the salmon spawning and rearing habitat and watershed resources at risk is simply unimaginable and unacceptable. Of particular concern is copper and other heavy metals in mine waste leaching into the Klehini River (shown) and the Chilkat River 14 miles downstream. Copper and heavy metals are toxic to salmon and bald eagles.<br />
<br />
The Chilkat River chum salmon are the primary food source for one of the largest gatherings of bald eagles in the world. Each fall, bald eagles congregate in the Alaska Chilkat Bald Eagle Preserve, located only three miles downriver from the area of current exploration.
    Klehini River Constantine Palmer Dep...jpg
  • A long line dangles from a helicopter above the location of the potential mine site being explored by Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan. The area of exploration, known as the Palmer Deposit is located near mile 40 of the Haines Highway and the Porcupine placer gold mining area near Haines, Alaska.<br />
<br />
The minerals that Constantine’s drilling explorations have found are primarily copper and zinc, with significant amounts of gold and silver. Exploratory drilling to refine the location and mineral amounts are the current focus of the company.<br />
<br />
If approved and developed, the mine would be an underground mine. Besides the actual ore deposits, having the nearby highway access for transporting ore to the deepwater port at Haines is also attractive to Constantine.<br />
<br />
Support for a large scale mine such as the Constantine project is divided among residents of Haines, a small community in Southeast Alaska 75 miles northwest of Juneau. The community’s needed economic boost from jobs, development and other mine support that a large-scale mine brings is tempting to some. To others, anything that might put the salmon spawning and rearing habitat and watershed resources at risk is simply unimaginable and unacceptable. Of particular concern is copper and other heavy metals in mine waste leaching into the Klehini and Chilkat River. Copper and heavy metals are toxic to salmon and bald eagles.<br />
<br />
The Chilkat River chum salmon are the primary food source for one of the largest gatherings of bald eagles in the world. Each fall, bald eagles congregate in the Alaska Chilkat Bald Eagle Preserve, located only three miles downriver from the area of current exploration. At times more than 3,000 eagles have been recorded at the primary gathering area for the fall chum salmon run.
    Helicopter working at Constantine Pa...jpg
  • The conflict over putting in a hard-rock mine near the Alaska Chilkat Bald Eagle Preserve near Haines, Alaska took a new turn recently with the filing of a lawsuit by an Alaska Native Tlingit tribe and three environmental groups. The group is suing the Bureau of Land Management, saying that the agency granted mineral exploration permits without considering how a mine could affect the Chilkat River's salmon and the Alaska Chilkat Bald Eagle Preserve. <br />
<br />
Joining the Tlingit village of Klukwan in the lawsuit against the Bureau of Land Management are the Southeast Alaska Conservation Council, Lynn Canal Conservation and Rivers Without Borders. They are represented by Earthjustice, a nonprofit environmental law firm. The group is asking for mining permits to be revoked.<br />
<br />
Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan is exploring a potential site for a mine (located center) just above Glacier Creek and the Klehini River near Haines Alaska. This area, known as the Palmer Deposit is located near mile 40 of the Haines Highway and the Porcupine placer gold mining area.<br />
<br />
Support for a large scale mine is divided among residents of Haines. The community’s needed economic boost from jobs that a large-scale mine brings is tempting to some. To others, anything that might put the salmon spawning and rearing habitat and watershed resources at risk is simply unimaginable and unacceptable. Of particular concern is copper and other heavy metals in mine waste leaching into the Klehini River (shown) and the Chilkat River 14 miles downstream. Copper and heavy metals are toxic to salmon and bald eagles.<br />
<br />
The Chilkat River chum salmon are the primary food source for one of the largest gatherings of bald eagles in the world. Each fall, bald eagles congregate in the Alaska Chilkat Bald Eagle Preserve, located only three miles downriver from the area of current exploration.
    Constantine Mine, Palmer Deposit.jpg
  • A spectacular display of the Aurora Borealis or as it is commonly called, the northern lights, occurred the evening of November 8 through the early morning of November 9, 2013 over Sinclair Mountain and other mountains in the Kakuhan Range at Haines, Alaska. The luminous glow in the upper atmosphere stretched across the skies above the Lynn Canal from Skagway to Juneau. The bottom edge of an aurora is typically 60 miles high with the top edge at an altitude of 120 to 200 miles, though sometimes high altitude aurora can be as high as 350 miles. The collision of sun storm electrons and protons with different types of gas particles in Earth’s atmosphere cause the different colors. Green, the most common color, is caused by the collision of electrons with atoms of with atomic oxygen. *** EDITORS NOTE: Boulders in foreground were lit with a flashlight during time exposure***
    Aurora Borealis over Haines, Alaska-...jpg
  • A spectacular display of the Aurora Borealis or as it is commonly called, the northern lights, occurred the evening of November 8 through the early morning of November 9, 2013 over Haines, Alaska. The luminous glow of the aurora borealis dances in the upper atmosphere above Mt. Emmerich and other peaks in the Chilkat Range at the Chilkat Inlet for the Chilkat River just outside Haines, Alaska. The bottom edge of an aurora is typically 60 miles high with the top edge at an altitude of 120 to 200 miles, though sometimes high altitude aurora can be as high as 350 miles. The collision of sun storm electrons and protons with different types of gas particles in Earth’s atmosphere cause the different colors. Green, the most common color, is caused by the collision of electrons with atoms of with atomic oxygen.
    Aurora Borealis over Haines, Alaska-...jpg
  • A spectacular display of the Aurora Borealis or as it is commonly called, the northern lights, occurred the evening of November 8 through the early morning of November 9, 2013 over Haines, Alaska. The luminous glow of the aurora borealis dances in the upper atmosphere above Mt. Emmerich and other peaks in the Chilkat Range at the Chilkat Inlet for the Chilkat River just outside Haines, Alaska. The bottom edge of an aurora is typically 60 miles high with the top edge at an altitude of 120 to 200 miles, though sometimes high altitude aurora can be as high as 350 miles. The collision of sun storm electrons and protons with different types of gas particles in Earth’s atmosphere cause the different colors. Green, the most common color, is caused by the collision of electrons with atoms of with atomic oxygen.
    Aurora Borealis over Haines, Alaska-...jpg
  • A spectacular display of the Aurora Borealis or as it is commonly called, the northern lights, occurred the evening of November 8 through the early morning of November 9, 2013 over Haines, Alaska. The luminous glow in the upper atmosphere stretched across the skies above the Lynn Canal from Skagway to Juneau. The bottom edge of an aurora is typically 60 miles high with the top edge at an altitude of 120 to 200 miles, though sometimes high altitude aurora can be as high as 350 miles. The collision of sun storm electrons and protons with different types of gas particles in Earth’s atmosphere cause the different colors. Green, the most common color, is caused by the collision of electrons with atoms of with atomic oxygen.
    Aurora Borealis over Haines, Alaska-...jpg
  • A spectacular display of the Aurora Borealis or as it is commonly called, the northern lights, occurred the evening of November 8 through the early morning of November 9, 2013 over Haines, Alaska. The luminous glow in the upper atmosphere stretched across the skies above the Lynn Canal from Skagway to Juneau. The bottom edge of an aurora is typically 60 miles high with the top edge at an altitude of 120 to 200 miles, though sometimes high altitude aurora can be as high as 350 miles. The collision of sun storm electrons and protons with different types of gas particles in Earth’s atmosphere cause the different colors. Green, the most common color, is caused by the collision of electrons with atoms of with atomic oxygen.
    Aurora Borealis over Haines, Alaska-...jpg
  • Fall foliage along the Trail of Time near the Mendenhall Glacier
    Trail of Time fall still life.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Anchorage Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide.jpg
  • A spectacular display of the Aurora Borealis or as it is commonly called, the northern lights, occurred the evening of November 8 through the early morning of November 9, 2013 over Sinclair Mountain and other mountains in the Kakuhan Range at Haines, Alaska. The luminous glow in the upper atmosphere stretched across the skies above the Lynn Canal from Skagway to Juneau. The bottom edge of an aurora is typically 60 miles high with the top edge at an altitude of 120 to 200 miles, though sometimes high altitude aurora can be as high as 350 miles. The collision of sun storm electrons and protons with different types of gas particles in Earth’s atmosphere cause the different colors. Green, the most common color, is caused by the collision of electrons with atoms of with atomic oxygen. *** EDITORS NOTE: Boulders in foreground were lit with a flashlight during time exposure***
    Northern lights over Haines, Alaska.jpg
  • Byers Peak-2.jpg
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