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  • 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
  • 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
  • The Black Tusk, located in Garibaldi Provincial Park of British Columbia, Canada, is the remains of an extinct stratovolcano. The 7,608 foot peak that is part of the Garibaldi Range of the Coast Mountains, is visible from the Whistler Blackcomb ski area, and along the Sea-to-Sky Highway, just south of Whistler. The lower portions of the Black Tusk are a popular backpacking and scrambling destination. Native Squamish legend says that the peak is where the mythical Thunderbird lives. In their native language it is known as t'ak't'ak mu'yin to’a in7in'a'xe7en (Landing Place of the Thunderbird).
    Black Tusk.jpg
  • The upper regions of the Tsirku and Buckwell Glaciers start in Tatshenshini-Alsek Provincial Park. The Tsirku Glacier (foreground) flows downward to become the Tsirku River, near Haines, Alaska and the Buckwell Glacier (upper right) flows to become Michael Creek which shortly connects with the O’Connor River. Tatshenshini-Alsek Provincial Park is located in the very northwestern corner of British Columbia, Canada. The park sits between Kluane National Park and Reserve in the Yukon and Glacier Bay and Wrangell-St. Elias National Parks and Preserves in Alaska. All together, they form the largest protected area in thew world, approximately 21 million acres. The Tatshenshini and Alsek Rivers are protected in their entirety making them the only large watershed in North America that is totally protected.<br />
<br />
The remote park is known for its spectacular glacier and icefields, rafting and kayaking, hiking and mountaineering. Tatshenshini-Alsek Provincial Park is home to grizzly bears, Dall's sheep, wolves, mountain goats, moose, eagles, falcons, and trumpeter swans.<br />
<br />
The park was designated a UNESCO World Heritage site in 1994.
    Tsirku Glacier and Tuckwell Glacier.jpg
  • The uppermost portion of the Grand Pacific Glacier appears like a road intersection in Tatshenshini-Alsek Provincial Park. The Grand Pacific Glacier flows downward toward the Gulf of Alaska in the flow in the top left, and downward to to the upper reach of Glacier Bay National Park in the bottom left and right flows. The top right flow is the Melbern Glacier. Tatshenshini-Alsek Provincial Park is located in the very northwestern corner of British Columbia, Canada. The park sits between Kluane National Park and Reserve in the Yukon and Glacier Bay and Wrangell-St. Elias National Parks and Preserves in Alaska. All together, they form the largest protected area in thew world, approximately 21 million acres. The Tatshenshini and Alsek Rivers are protected in their entirety making them the only large watershed in North America that is totally protected.<br />
<br />
The remote park is known for its spectacular glacier and icefields, rafting and kayaking, hiking and mountaineering. Tatshenshini-Alsek Provincial Park is home to grizzly bears, Dall's sheep, wolves, mountain goats, moose, eagles, falcons, and trumpeter swans.<br />
<br />
The park was designated a UNESCO World Heritage site in 1994.
    Grand Pacific Glacier crossroad.jpg
  • Stawamus Chief, a huge granite dome, is located near Squamish, British Columbia, Canada. Towering over 2,297 feet above nearby Howe Sound and the Sea-to-Sky Highway, it is a popular, world-class climbing destination along with other climbing spots in the Squamish area.
    Stawamus Chief.jpg
  • The curved stainless-steel exterior of the Walt Disney Concert Hall located in downtown Los Angeles was designed by architect Frank Gehry. The Disney Concert Hall, opened in 2003
    Disney Concert Hall exterior detail.jpg
  • The Black Tusk, located in Garibaldi Provincial Park of British Columbia, Canada, is the remains of an extinct stratovolcano. The 7,608 foot peak that is part of the Garibaldi Range of the Coast Mountains, is visible from the Whistler Blackcomb ski area, and along the Sea-to-Sky Highway, just south of Whistler. The lower portions of the Black Tusk are a popular backpacking and scrambling destination. Native Squamish legend says that the peak is where the mythical Thunderbird lives. In their native language it is known as t'ak't'ak mu'yin to’a in7in'a'xe7en (Landing Place of the Thunderbird).
    Black Tusk.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
  • 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 upper right) just above Glacier Creek (not visible) and the Klehini River (foreground), 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 />
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.
    Klehini River 2.jpg
  • Hallett Peak (12,720 feet) looms above Bear Lake. Carol and I climbed to the top of the peak in our younger years. It wasn’t quite as hard as it looks. We climbed it from the west side of the Continental Divide. #routefinding
    Hallett Peak and Bear Lake.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 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
  • 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 Palmer Deposit...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 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
  • Hallett Peak  (12,720 feet) looms above a frozen Bear Lake in Rocky Mountain National Park in March.
    Hallett Peak and Bear Lake-3.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
  • 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 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 />
This aerial photo of the Lamplugh Glacier landslide was taken two days after the landslide.
    Lamplugh Glacier landslide-5.jpg
  • An American black bear (Ursus americanus), eats dandelions just outside the boundary of Kluane National Park and Preserve along Yukon Highway 3, near Gribbles Gulch in the Yukon Territory, Canada. While most of a black bear’s diet is vegetation, black bears are omnivores meaning that they eat both plants and animals (grasses, berries, roots, insects, fish and mammals). Black bears typically weight 200 to 600 pounds. Not all black bears are black in color -- some are brown or even blond. They are most easily distinguished apart from grizzly bears by the lack of the pronounced shoulder hump found in a grizzly bear. The black bear is not considered to be a threatened species, though care to keep them from getting human food and garbage is needed to protect them from conflicts with humans. Kluane National Park and Reserve is known for it's  massive mountains, spectacular glacier and icefield landscapes including Canada's tallest peak, Mount Logan (19,545 ft.). The 5.4 million acre park is also known for it's wildlife, including grizzly bears, wolves, caribou and Dall sheep. The park is one of a collection of U.S. and Canadian national and provincial parks that form the largest international protected area in the world. Kluane National Park and Reserve was selected as a UNESCO World Heritage Site for being an outstanding wilderness of global significance. EDITORS NOTE: Image is a slightly cropped version of Image ID: I0000xjOvlNPfAYk
    Black bear eating dandelions - 5.jpg
  • An American black bear (Ursus americanus), eats dandelions just outside the boundary of Kluane National Park and Preserve along Yukon Highway 3, near Gribbles Gulch in the Yukon Territory, Canada. While most of a black bear’s diet is vegetation, black bears are omnivores meaning that they eat both plants and animals (grasses, berries, roots, insects, fish and mammals). Black bears typically weight 200 to 600 pounds. Not all black bears are black in color -- some are brown or even blond. They are most easily distinguished apart from grizzly bears by the lack of the pronounced shoulder hump found in a grizzly bear. The black bear is not considered to be a threatened species, though care to keep them from getting human food and garbage is needed to protect them from conflicts with humans. Kluane National Park and Reserve is known for it's  massive mountains, spectacular glacier and icefield landscapes including Canada's tallest peak, Mount Logan (19,545 ft.). The 5.4 million acre park is also known for it's wildlife, including grizzly bears, wolves, caribou and Dall sheep. The park is one of a collection of U.S. and Canadian national and provincial parks that form the largest international protected area in the world. Kluane National Park and Reserve was selected as a UNESCO World Heritage Site for being an outstanding wilderness of global significance. EDITORS NOTE: Image is a slightly cropped version of Image ID: I0000BKcCs4KBkEw.
    Black bear eating dandelions - 3.jpg
  • Pictured is the cornerstone of the abandoned Clements Stone Arch Bridge over the Cottonwood River is located in the Kansas Flint Hills approximately 1/2 mile south of Clements, south of highway US 50 near the Flying W Ranch in Chase County. The bridge with its massive 28 foot double arches is the largest and one of the oldest limestone bridges in Kansas. Built in 1886 though not completed until 1888, the bridge was placed on the National Register of Historic Places in 1976. Today, the bridge no longer carries traffic and seems out of place now that the road over the bridge ends up into a pasture.
    Clements Stone Arch Bridge cornersto...jpg
  • The massive 60 x 110 foot three-story limestone barn on the Spring Hill Farm and Stock Ranch located in the Tallgrass Prairie National Preserve in the Kansas Flint Hills was built by cattleman Stephen F. Jones. The bottom level is built into the side of a hill for insulation and the second level is even with the top of the hill for access. The 10,894-acre Tallgrass Prairie National Preserve is located in Chase County near the towns of Strong City and Cottonwood Falls. Less than four percent of the original 140 million acres of tallgrass prairie remains in North America. Most of the remaining tallgrass prairie is in the Flint Hills in Kansas. Tallgrass Prairie National Preserve is the only unit of the National Park Service dedicated to the preservation of the tallgrass prairie ecosystem. The Tallgrass Prairie National Preserve is co-managed with The Nature Conservancy.
    Spring Hill barn.jpg
  • An American black bear (Ursus americanus), eats dandelions just outside the boundary of Kluane National Park and Preserve along Yukon Highway 3, near Gribbles Gulch in the Yukon Territory, Canada. While most of a black bear’s diet is vegetation, black bears are omnivores meaning that they eat both plants and animals (grasses, berries, roots, insects, fish and mammals). Black bears typically weight 200 to 600 pounds. Not all black bears are black in color -- some are brown or even blond. They are most easily distinguished apart from grizzly bears by the lack of the pronounced shoulder hump found in a grizzly bear. The black bear is not considered to be a threatened species, though care to keep them from getting human food and garbage is needed to protect them from conflicts with humans. Kluane National Park and Reserve is known for it's  massive mountains, spectacular glacier and icefield landscapes including Canada's tallest peak, Mount Logan (19,545 ft.). The 5.4 million acre park is also known for it's wildlife, including grizzly bears, wolves, caribou and Dall sheep. The park is one of a collection of U.S. and Canadian national and provincial parks that form the largest international protected area in the world. Kluane National Park and Reserve was selected as a UNESCO World Heritage Site for being an outstanding wilderness of global significance.
    Black bear eating dandelions - 1.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 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.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
  • An American black bear (Ursus americanus), eats dandelions just outside the boundary of Kluane National Park and Preserve along Yukon Highway 3, near Gribbles Gulch in the Yukon Territory, Canada. While most of a black bear’s diet is vegetation, black bears are omnivores meaning that they eat both plants and animals (grasses, berries, roots, insects, fish and mammals). Black bears typically weight 200 to 600 pounds. Not all black bears are black in color -- some are brown or even blond. They are most easily distinguished apart from grizzly bears by the lack of the pronounced shoulder hump found in a grizzly bear. The black bear is not considered to be a threatened species, though care to keep them from getting human food and garbage is needed to protect them from conflicts with humans. Kluane National Park and Reserve is known for it's  massive mountains, spectacular glacier and icefield landscapes including Canada's tallest peak, Mount Logan (19,545 ft.). The 5.4 million acre park is also known for it's wildlife, including grizzly bears, wolves, caribou and Dall sheep. The park is one of a collection of U.S. and Canadian national and provincial parks that form the largest international protected area in the world. Kluane National Park and Reserve was selected as a UNESCO World Heritage Site for being an outstanding wilderness of global significance. EDITORS NOTE: Image is a slightly cropped version of Image ID: I0000hi_N20NHKOQ.
    Black bear eating dandelions - 2.jpg
  • The abandoned Clements Stone Arch Bridge over the Cottonwood River is located in the Kansas Flint Hills approximately 1/2 mile south of Clements, south of highway US 50 near the Flying W Ranch in Chase County. The bridge with its massive 28 foot double arches is the largest and one of the oldest limestone bridges in Kansas. Built in 1886 though not completed until 1888, the bridge was placed on the National Register of Historic Places in 1976. Today, the bridge no longer carries traffic and seems out of place now that the road over the bridge ends up into a pasture.
    Clements Stone Arch Bridge-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.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-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 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 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
  • 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
  • An American black bear (Ursus americanus), eats dandelions just outside the boundary of Kluane National Park and Preserve along Yukon Highway 3, near Gribbles Gulch in the Yukon Territory, Canada. While most of a black bear’s diet is vegetation, black bears are omnivores meaning that they eat both plants and animals (grasses, berries, roots, insects, fish and mammals). Black bears typically weight 200 to 600 pounds. Not all black bears are black in color -- some are brown or even blond. They are most easily distinguished apart from grizzly bears by the lack of the pronounced shoulder hump found in a grizzly bear. The black bear is not considered to be a threatened species, though care to keep them from getting human food and garbage is needed to protect them from conflicts with humans. Kluane National Park and Reserve is known for it's  massive mountains, spectacular glacier and icefield landscapes including Canada's tallest peak, Mount Logan (19,545 ft.). The 5.4 million acre park is also known for it's wildlife, including grizzly bears, wolves, caribou and Dall sheep. The park is one of a collection of U.S. and Canadian national and provincial parks that form the largest international protected area in the world. Kluane National Park and Reserve was selected as a UNESCO World Heritage Site for being an outstanding wilderness of global significance. EDITORS NOTE: Image is a slightly cropped version of Image ID: I0000o_hJgKSbYFg
    Black bear eating dandelions - 7.jpg
  • An American black bear (Ursus americanus), eats dandelions just outside the boundary of Kluane National Park and Preserve along Yukon Highway 3, near Gribbles Gulch in the Yukon Territory, Canada. While most of a black bear’s diet is vegetation, black bears are omnivores meaning that they eat both plants and animals (grasses, berries, roots, insects, fish and mammals). Black bears typically weight 200 to 600 pounds. Not all black bears are black in color -- some are brown or even blond. They are most easily distinguished apart from grizzly bears by the lack of the pronounced shoulder hump found in a grizzly bear. The black bear is not considered to be a threatened species, though care to keep them from getting human food and garbage is needed to protect them from conflicts with humans. Kluane National Park and Reserve is known for it's  massive mountains, spectacular glacier and icefield landscapes including Canada's tallest peak, Mount Logan (19,545 ft.). The 5.4 million acre park is also known for it's wildlife, including grizzly bears, wolves, caribou and Dall sheep. The park is one of a collection of U.S. and Canadian national and provincial parks that form the largest international protected area in the world. Kluane National Park and Reserve was selected as a UNESCO World Heritage Site for being an outstanding wilderness of global significance.
    Black bear eating dandelions - 4.jpg
  • An American black bear (Ursus americanus), eats dandelions just outside the boundary of Kluane National Park and Preserve along Yukon Highway 3, near Gribbles Gulch in the Yukon Territory, Canada. While most of a black bear’s diet is vegetation, black bears are omnivores meaning that they eat both plants and animals (grasses, berries, roots, insects, fish and mammals). Black bears typically weight 200 to 600 pounds. Not all black bears are black in color -- some are brown or even blond. They are most easily distinguished apart from grizzly bears by the lack of the pronounced shoulder hump found in a grizzly bear. The black bear is not considered to be a threatened species, though care to keep them from getting human food and garbage is needed to protect them from conflicts with humans. Kluane National Park and Reserve is known for it's  massive mountains, spectacular glacier and icefield landscapes including Canada's tallest peak, Mount Logan (19,545 ft.). The 5.4 million acre park is also known for it's wildlife, including grizzly bears, wolves, caribou and Dall sheep. The park is one of a collection of U.S. and Canadian national and provincial parks that form the largest international protected area in the world. Kluane National Park and Reserve was selected as a UNESCO World Heritage Site for being an outstanding wilderness of global significance.
    Black bear eating dandelions - 1.jpg
  • Kayakers are dwarfed by the massive Holgate Glacier at sunset on the Holgate Arm of Aialik Bay in Kenai Fjords National Park in Alaska. Photo was taken from the Holgate public use cabin. The park, located near Seward, Alaska, is known for its glaciers that flow out from the Harding Icefield, and the coastal fjords shaped by its receding glaciers. Approximately 51 percent of the park is covered by ice. The Harding Icefield, thousands of feet deep, is the largest icefield solely contained within the United States. Exit Glacier, is one of the most accessible glaciers in Alaska with easy walking trails leading up to the face of the glacier and more difficult trails leading up to the Harding Icefield which feeds Exit Glacier. Abundant land and sea life can be found within the parks boundaries including black and grizzly bears, Steller sea lions, puffins, humpback and orca whales. The park is a popular destination with sea kayakers who frequent Aialik Bay, Holgate Arm, Pederson Lagoon and Northwestern Fjord for magnificent views of the Aialik, Holgate, and Pederson glaciers. Tour companies offer boat tours out of Seward.
    Holgate Glacier kayakers, Aialik Bay...jpg
  • Close up of the stones of the abandoned Clements Stone Arch Bridge over the Cottonwood River is located in the Kansas Flint Hills approximately 1/2 mile south of Clements, south of highway US 50 near the Flying W Ranch in Chase County. The bridge with its massive 28 foot double arches is the largest and one of the oldest limestone bridges in Kansas. Built in 1886 though not completed until 1888, the bridge was placed on the National Register of Historic Places in 1976. Today, the bridge no longer carries traffic and seems out of place now that the road over the bridge ends up into a pasture.
    Clements Stone Arch Bridge stones.jpg
  • The abandoned Clements Stone Arch Bridge over the Cottonwood River is located in the Kansas Flint Hills approximately 1/2 mile south of Clements, south of highway US 50 near the Flying W Ranch in Chase County. The bridge with its massive 28 foot double arches is the largest and one of the oldest limestone bridges in Kansas. Built in 1886 though not completed until 1888, the bridge was placed on the National Register of Historic Places in 1976. Today, the bridge no longer carries traffic and seems out of place now that the road over the bridge ends up into a pasture.
    Clements Stone Arch Bridge-3.jpg
  • The abandoned Clements Stone Arch Bridge over the Cottonwood River is located in the Kansas Flint Hills approximately 1/2 mile south of Clements, south of highway US 50 near the Flying W Ranch in Chase County. The bridge with its massive 28 foot double arches is the largest and one of the oldest limestone bridges in Kansas. Built in 1886 though not completed until 1888, the bridge was placed on the National Register of Historic Places in 1976. Today, the bridge no longer carries traffic and seems out of place now that the road over the bridge ends up into a pasture.
    Clements Stone Arch Bridge.jpg
  • The abandoned Clements Stone Arch Bridge over the Cottonwood River is located in the Kansas Flint Hills approximately 1/2 mile south of Clements, south of highway US 50 near the Flying W Ranch in Chase County. The bridge with its massive 28 foot double arches is the largest and one of the oldest limestone bridges in Kansas. Built in 1886 though not completed until 1888, the bridge was placed on the National Register of Historic Places in 1976. Today, the bridge no longer carries traffic and seems out of place now that the road over the bridge ends up into a pasture.
    Clements Stone Arch Bridge.jpg
  • Visitors to Mendenhall Glacier near Juneau, Alaska hike the short and easy Photo Point Trail for a look at icebergs from the Mendenhall Glacier. The glacier descends from the massive Juneau Icefield into Mendenhall Lake. Mendenhall Glacier is a popular spot for cruise ship passengers and it sees over 500,000 visitors a year.
    Mendenhall Glacier.jpg
  • Some of the large boulders known as the “Jigsaw Blocks" located on the Lost Valley Trail near the Buffalo River and Ponca, Arkansas. The massive limestone blocks are the result of corrosion and erosion of the rock face the bluffs along Clark Creek.<br />
<br />
The 150-mile Buffalo River in northern Arkansas was the first river in the United States to receive the designation as a National River. The Buffalo National River, encompasses 135 miles of the river which is managed by the National Park Service. The river is a popular canoeing, kayaking, camping, and fishing destination. Popular destinations in the national river’s boundaries include; Lost Valley, Hemmed-In-Hollow Falls (the highest waterfall between the Appalachian and Rocky Mountains, Indian Rockhouse, numerous caves and over 500-foot tall bluffs. The area is also home to Arkansas’ only elk herd.
    Jigsaw Blocks-2.jpg
  • A hiker passes by the large boulders known as the “Jigsaw Blocks" located on the Lost Valley Trail near the Buffalo River and Ponca, Arkansas. The massive limestone blocks are the result of corrosion and erosion of the rock face the bluffs along Clark Creek.<br />
<br />
The 150-mile Buffalo River in northern Arkansas was the first river in the United States to receive the designation as a National River. The Buffalo National River, encompasses 135 miles of the river which is managed by the National Park Service. The river is a popular canoeing, kayaking, camping, and fishing destination. Popular destinations in the national river’s boundaries include; Lost Valley, Hemmed-In-Hollow Falls (the highest waterfall between the Appalachian and Rocky Mountains, Indian Rockhouse, numerous caves and over 500-foot tall bluffs. The area is also home to Arkansas’ only elk herd.
    Jigsaw Blocks.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
  • An American black bear (Ursus americanus), eats dandelions just outside the boundary of Kluane National Park and Preserve along Yukon Highway 3, near Gribbles Gulch in the Yukon Territory, Canada. While most of a black bear’s diet is vegetation, black bears are omnivores meaning that they eat both plants and animals (grasses, berries, roots, insects, fish and mammals). Black bears typically weight 200 to 600 pounds. Not all black bears are black in color -- some are brown or even blond. They are most easily distinguished apart from grizzly bears by the lack of the pronounced shoulder hump found in a grizzly bear. The black bear is not considered to be a threatened species, though care to keep them from getting human food and garbage is needed to protect them from conflicts with humans. Kluane National Park and Reserve is known for it's  massive mountains, spectacular glacier and icefield landscapes including Canada's tallest peak, Mount Logan (19,545 ft.). The 5.4 million acre park is also known for it's wildlife, including grizzly bears, wolves, caribou and Dall sheep. The park is one of a collection of U.S. and Canadian national and provincial parks that form the largest international protected area in the world. Kluane National Park and Reserve was selected as a UNESCO World Heritage Site for being an outstanding wilderness of global significance.
    Black bear eating dandelions - 8.jpg
  • An American black bear (Ursus americanus), eats dandelions just outside the boundary of Kluane National Park and Preserve along Yukon Highway 3, near Gribbles Gulch in the Yukon Territory, Canada. While most of a black bear’s diet is vegetation, black bears are omnivores meaning that they eat both plants and animals (grasses, berries, roots, insects, fish and mammals). Black bears typically weight 200 to 600 pounds. Not all black bears are black in color -- some are brown or even blond. They are most easily distinguished apart from grizzly bears by the lack of the pronounced shoulder hump found in a grizzly bear. The black bear is not considered to be a threatened species, though care to keep them from getting human food and garbage is needed to protect them from conflicts with humans. Kluane National Park and Reserve is known for it's  massive mountains, spectacular glacier and icefield landscapes including Canada's tallest peak, Mount Logan (19,545 ft.). The 5.4 million acre park is also known for it's wildlife, including grizzly bears, wolves, caribou and Dall sheep. The park is one of a collection of U.S. and Canadian national and provincial parks that form the largest international protected area in the world. Kluane National Park and Reserve was selected as a UNESCO World Heritage Site for being an outstanding wilderness of global significance.
    Black bear eating dandelions - 6.jpg