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  • The Muir Inlet of the East Arm of Glacier Bay in Glacier Bay National Park and Preserve offers some of the best sea kayaking in the park. The turquoise color of the water is caused by the minerals contained in “rock flour;” the material that tidewater glaciers release as the glaciers grind rocks into dust on their way to the sea. This aerial view is looking south, down the Muir Inlet. Pictured are: The Nunatak and Nunatak Cove (left foreground); Westdahl Point (right foreground), Stump Cove, the entrance to Wachusett Inlet; Hunter Cove, Rowlee Point, Point McLeod (middle right); Sealers Island (enter); Maquinna Cove (center background); Adams Inlet (center background to left background); Tree Mountain, Mount Case, Mount Right; Garforth Island, Sturgess Island, North Marble Island, South Marble Island, Willoughby Island, the northernmost islands of the Beardslee Island (upper right background); Sitakaday Narrows and the entrance to Glacier Bay (furthermost upper right background).<br />
<br />
Glacier Bay National Park and Preserve 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. The effects of a warming climate are easily seen here. It is a place where can you witness geological change firsthand — change that is normally measured in millennia.
    Muir Inlet aerial of East Arm.jpg
  • The Muir Inlet of the East Arm of Glacier Bay in Glacier Bay National Park and Preserve offers some of the best sea kayaking in the park. The turquoise color of the water is caused by the minerals contained in “rock flour;” the material that tidewater glaciers release as the glaciers grind rocks into dust on their way to the sea. This aerial view is looking south, down the Muir Inlet. Pictured are: The Nunatak and Nunatak Cove (left foreground); Westdahl Point (right foreground), Stump Cove, the entrance to Wachusett Inlet; Hunter Cove, Rowlee Point, Point McLeod (middle right); Sealers Island (enter); Maquinna Cove (center background); Adams Inlet (center background to left background); Tree Mountain, Mount Case, Mount Right; Garforth Island, Sturgess Island, North Marble Island, South Marble Island, Willoughby Island, the northernmost islands of the Beardslee Island (upper right background); Sitakaday Narrows and the entrance to Glacier Bay (furthermost upper right background).<br />
<br />
Glacier Bay National Park and Preserve 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. The effects of a warming climate are easily seen here. It is a place where can you witness geological change firsthand — change that is normally measured in millennia.
    Muir Inlet aerial of East Arm.jpg
  • The dark intertidal zone is contrasted against snow along the beaches in this aerial photo of the Chilkat Peninsula near Haines, Alaska after a snow storm. Pictured at lower left is the Letnikof Cove Cannery in this view looking south, down the Chilkat and Chilkoot Inlets towards the Lynn Canal. In the background are the mountains of the Kakuhan Range. The small snow covered bay at upper left is known locally as Mud Bay.
    Chilkat Peninsula aerial.jpg
  • The thousand foot cliffs of White Thunder Ridge are reflected in the Muir Inlet located in Glacier Bay National Park and Preserve in southeast Alaska. This aerial view, taken in early November after a snow storm, is looking south, down the Muir Inlet (left).
    White Thunder Ridge aerial.jpg
  • The upper snowfield of the Casement Glacier is seen in this aerial photo taken along the border of Glacier Bay National Park and Preserve near Mount Rice and the town of Haines in southeast Alaska.
    Casement Glacier icefield aerial.jpg
  • The retreating McBride Glacier, located just off the Muir Inlet in Glacier Bay National Park and Preserve in southeast Alaska, is the most active glacier and only tidewater glacier in the Muir Inlet. McBride Glacier is approximately 1⁄2 mile wide and 14 miles long. Its ice face is approximately 200 feet high above the water and extends about 270 feet below it. This aerial photo, shot after an early November snow storm, shows Icebergs from the calving glacier traveling down the McBride Glacier inlet to the main Muir Inlet (background). The mountain ridge (center right) is McConnell Ridge. Ridge to the left is of McBride Inlet is Van Horn Ridge.
    McBride Glacier aerial 2.jpg
  • The retreating McBride Glacier, located just off the Muir Inlet in Glacier Bay National Park and Preserve in southeast Alaska, is the most active glacier and only tidewater glacier in the Muir Inlet. McBride Glacier is approximately 1⁄2 mile wide and 14 miles long. Its ice face is approximately 200 feet high above the water and extends about 270 feet below it. This aerial photo, shot after an early November snow storm, shows Icebergs from the calving glacier traveling down the McBride Glacier inlet to the main Muir Inlet. The mountain ridge at left foreground is McConnell Ridge.
    McBride Glacier aerial.jpg
  • The upper snowfield of the Casement Glacier is seen in this aerial photo taken along the border of Glacier Bay National Park and Preserve near Mount Rice and the town of Haines in southeast Alaska.
    Casement Glacier snowfield aerial 2.jpg
  • This aerial photo of the upper Chilkat River valley taken above Mosquito Lake shows the upper portion of the Alaska Chilkat Bald Eagle Preserve. At upper left is the Kelsall River valley. Identifiable mountains include: Hiteshitak Mountain (left of center), Tohikah Mountain (center), and Mount Raymond (rear right in sunlight area). During late fall, bald eagles congregate along the Chilkat River to feed on salmon. This gathering of bald eagles in the Alaska Chilkat Bald Eagle Preserve is believed to be one of the largest gatherings of bald eagles in the world.
    Upper Chilkat River valley aerial.jpg
  • The many braids of the Chilkat River are visible in this aerial photo of the river taken near Haines, Alaska. The Chilkat River is a popular destination for photographers who come to the river in November and December to photograph one of the largest gatherings of bald eagles in the world.
    Chilkat River aerial.jpg
  • Pyramid Island, stands as a sentinel to the Chilkat River valley where the Chilkat River reaches the ocean and becomes the Chilkat Inlet. The Chilkat River, located outside Haines, Alaska, is a popular destination for photographers who come to the river in November and December to photograph one of the largest gatherings of bald eagles in the world. This aerial photo is looking up the river valley from Haines. Mountains of the Takshanuk Range that are visible include Mount Ripinski (right) and Tukgahgo Mountain (center). The tidal flats area just beyond Pyramid Island are known as McClellan Flats.
    Pyramid Island, Chilkat River aerial.jpg
  • The retreating McBride Glacier, located just off the Muir Inlet in Glacier Bay National Park and Preserve in southeast Alaska, is the most active glacier and only tidewater glacier in the Muir Inlet. McBride Glacier is approximately 1⁄2 mile wide and 14 miles long. Its ice face is approximately 200 feet high above the water and extends about 270 feet below it. This aerial photo, shot after an early November snow storm, shows Icebergs from the calving glacier traveling down the McBride Glacier inlet to the main Muir Inlet. The mountain ridge in the center is McConnell Ridge.
    McBride Glacier, icebergs aerial.jpg
  • An unamed mountain peak on Takhin Ridge towers above the Takhin River in southeast Alaska near Haines. The peak, seen in this aerial photo is near Chunekukleik Mountain (not visible in photo).
    Takhin Ridge, Takhin River aerial.jpg
  • The Chilkat River valley outside Haines, Alaska is a popular destination for photographers who come to the river in November and December to photograph one of the largest gatherings of bald eagles in the world. This aerial photo is looking up the river valley from Haines to the Alaska Chilkat Bald Eagle Preserve and further to the border with Canada. Four Winds Mountain is located on the left and the Takshanuk Range on the right.
    Chilkat River valley aerial.jpg
  • The dark intertidal zone of the McClellan Flats of the Chilkat Inlet is contrasted against snow and ice on the Chilkat River in this aerial photo taken just outside Haines in southeast Alaska. The Chilkat River is a popular destination for photographers who come to the river in November and December to photograph one of the largest gatherings of bald eagles in the world.
    Chilkat River tidal zone aerial, Hai...jpg
  • The Chilkoot River corridor between Chilkoot Lake (upper left) and Lutak Inlet of the Lynn Canal (bottom right) is a popular sport fishing spot and a culturally important Tlingit historic site. The river area is also popular with grizzly bears who also come for the salmon who spawn in the Chilkoot River. While this concentration of bears makes for exciting bear viewing for visitors, the narrow corridor in which humans and bears must pass can lead to dangerous encounters. The Alaska Legislature has approved $1 million for a bear-viewing platform aimed at reducing encounters between bears and visitors to the scenic corridor. This area is part of the popular Chilkoot Lake State Recreation Site. In the upper reaches of the Chilkoot River Valley (not pictured) there have been proposals to dam the outlet of Connelly Lake, a high alpine lake above the Chilkoot River, for a hydroelectric project. Environmental concerns include the impact construction and project operation would have on fish spawning and rearing habitat (water turbidity issues), and bald eagles. Alaska Power and Telephone announced in June 2013 that it was putting the project on hold citing difficulty securing funding from the Alaska Energy Authority and the lack of community support. Despite these setbacks AP&T says that it not abandoning pursuing the project. In early September 2013, the Haines Borough announced that it was exploring possibly filing for a preliminary permit now that the project was no longer being pursued by AP&T.
    Chilkoot River aerial.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 (left). 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 -3.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 on the steep mountain slopes shown in this photo. This 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. Exploratory drilling to refine the location and mineral amounts are the current focus of the company.<br />
<br />
If approved and developed, the mine, near Haines, Alaska 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. The Haines Highway can be seen in photo on the right.<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 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 -6.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
  • Takhin Ridge (left) towers over the Takhin River in southeast Alaska near Haines. The Takhin River flows into the Chilkat River which is located at the base of the Takshanuk Mountains seen in background.
    Takhin River, Takhin Ridge aerial.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
  • Porcupine Peak (upper right) looks down on McKinley Creek. Just below the farm of this image, Mckinley Creek flows into Porcupine Creek, a placer gold mining stream. The area pictured is part of land from the Alaska Mental Health Trust being leased by Constantine Metal Resources Ltd. for mineral rights only. Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan is exploring a nearby potential site for a mine known as the Palmer Deposit.
    McKinley Creek aerial.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 on the steep mountain slopes shown in this photo. This 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. Exploratory drilling to refine the location and mineral amounts are the current focus of the company.<br />
<br />
If approved and developed, the mine, near Haines, Alaska 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. The Haines Highway can be seen in photo on the right.<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 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 -5.jpg
  • Chilkat Lake is located between Takhin Ridge (right) and the Chilkat River (left). In the distance (upper left) is the Chilkat Peninsula where the town of Haines is located. The tallest peak (center right) is Mount Emmerich. While a portion (foreground area) of Chilkat Lake is located in the Alaska Chilkat Bald Eagle Preserve, most of the preserve is located on the Chilkat River.
    Chilkat Lake aerial.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 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
  • 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 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 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 />
This aerial photo of the Lamplugh Glacier landslide was taken two days after the landslide.
    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
  • 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
  • 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 (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 Takhin Ridge and Takhinsha Mountains. Chilkat Lake is pictured on the left, below the mountains.
    Tsirku River alluvial fan with Chilk...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 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-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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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
  • 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 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
  • 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
  • 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 significant portion of the Haines State Forest pictured in this photo is under consideration for harvest. Known as the Baby Brown Timber Sale, the proposal by the Alaska Division of Forestry calls for 1,000 acres (20 million board feet) of Sitka spruce and  western hemlock to be harvested from state land. This photo shows a portion of the Baby Brown Timber Sale area near Haines Alaska between Glacier Creek (bottom), and Jarvis Creek (top). The Klehini River is at the right. Also visible is the Haines Highway (AK-7). The Baby Brown Timber Sale also includes forest land west of Porcupine Creek (not shown).<br />
<br />
The area pictured also shows land that Constantine Metal Resources Ltd. has leased mineral rights. Constantine Metals is also currently exploring the area above Glacier Creek. The minerals that Constantine’s drilling explorations have found are primarily copper and zinc, with significant amounts of gold and silver.<br />
<br />
If approved, the Baby Brown Timber Sale would be the largest sale in the Chilkat Valley since the 1990’s. The Division of Forestry estimates that the sale could generate 20 jobs directly associated with the harvest, $300,000 in royalties to the state. The economic impact of the sale to the statewide economy is estimated to $2,000,000.<br />
<br />
Conservation groups are concerned by the size of the sale and the impact a sale of this size will have on the watershed, fish, and wildlife. There are also concerns about the impact the harvest will have on the viewshed visible from the Haines Highway (AK-7) which has been designated as a National Scenic Byway.
    Baby Brown Timber Sale.jpg
  • A small glacial lake adds bright color to the otherwise bright white Tsirku Glacier in Tatshenshini-Alsek Provincial Park. The park, located in the very northwestern corner of British Columbia, Canada, 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.
    Small glacial lake-2.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 land in eastern Washington along the Snake River appears to be dry in this photo taken at 1:12 p.m. on an Alaska Airlines flight from Seattle-Tacoma International Airport to St. Louis, Mo. At the time this photo was taken on July 31,2017 the state of Washington was experiencing very dry conditions. In Seattle, <br />
<br />
Seattle’s record-breaking 55-day dry streak would later end on Aug. 12, when 0.02″ of rain fell. This was the first time measurable precipitation was recorded in the city since June 17.
    Dry conditions along the Snake River...jpg
  • The shadow of a DeHaviland DHC-2 Beaver travels perfectly down the runway at the Haines Airport in southeast Alaska. The plane, belonging to Haines-based Mountain Flying Service was taking off for a flightseeing tour to nearby Glacier Bay National Park and Preserve.
    Shadow of plane taking off.jpg
  • A small glacial lake adds bright color to the otherwise bright white Tsirku Glacier in Tatshenshini-Alsek Provincial Park. The park, located in the very northwestern corner of British Columbia, Canada, 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.
    Small glacial lake.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
  • 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 />
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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 />
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The park was designated a UNESCO World Heritage site in 1994.
    Tsirku Glacier and Tuckwell Glacier.jpg
  • Among the major highways that connect Los Angeles to the rest of the nation is U.S. Route 101, which travels the California, Oregon and Washington coasts for 1,550 miles. This image of the highway and downtown Los Angeles was taken from the Jerome C. Daniel Overlook.<br />
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Los Angeles, located on the Pacific Ocean in southern California, is the second-most populous city in the United States. It is the regions business and cultural center, most famously known for the entertainment, television, and motion picture industries.
    U.S. Route 101 Los Angeles.jpg
  • A landslide spilled onto the Ferris Glacier in Tatshenshini-Alsek Provincial Park. 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 />
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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 />
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The park was designated a UNESCO World Heritage site in 1994.
    Ferris Glacier landslide.jpg
  • Connelly Lake (center) is a 90-acre alpine lake near Haines, Alaska that drains into the Chilkoot River. Connelly Lake is the focus of a proposed $32 million, 12-megawatt hydroelectric project by Alaska Power and Telephone Company (AP&T). AP&T proposes to build a dam at the outlet of Connelly Lake that would create a 160-acre reservoir and a 6,200-foot-long penstock down the side of the mountain where water would be delivered to turbine generators located in a powerhouse near the Chilkoot River into which the lake water would be discharged. Some of the main features of the proposed Connelly Lake project (for example portions of the penstock, the powerhouse, access roads, and the transmission line) would be located in the Alaska Chilkat Bald Eagle Preserve and the Haines State Forest. Concerns include the impact construction and project operation would have on fish spawning and rearing habitat, and bald eagles. The eagles rely on the salmon that use the Chilkoot Valley in the fall and early winter when they are attracted to late spawning salmon runs. A hydro aquatic studies report prepared by the Shipley Group states that according to the Alaska Department of Fish and Game, 41 percent of the sockeye salmon in the upper Lynn Canal come from the Chilkoot River with 25 percent of those salmon spawning in the Chilkoot River drainage above Chilkoot Lake. The value of the fishery is estimated at more than $1,000,000 annually. AP&T announced in June 2013 that it was putting the project on hold citing difficulty securing funding from the Alaska Energy Authority and the lack of community support. Despite these setbacks AP&T says that it not abandoning pursuing the project. In early September 2013, the Haines Borough announced that it was exploring possibly filing for a preliminary permit now that the project was no longer being pursued by AP&T. This photo of the ice and snow covered Connelly Lake was taken in mid-July.
    Connelly Lake, Chilkoot River - 1.jpg
  • Snow-covered Connelly Lake (foreground left) is a 90-acre alpine lake near Haines, Alaska that drains into the Chilkoot River (right). Connelly Lake is the focus of a proposed $32 million, 12-megawatt hydroelectric project by Alaska Power and Telephone Company (AP&T). AP&T proposes to build a dam at the outlet of Connelly Lake that would create a 160-acre reservoir and a 6,200-foot-long penstock down the side of the mountain where water would be delivered to turbine generators located in a powerhouse near the Chilkoot River into which the lake water would be discharged. Some of the main features of the proposed Connelly Lake project (for example portions of the penstock, the powerhouse, access roads, and the transmission line) would be located in the Alaska Chilkat Bald Eagle Preserve and the Haines State Forest. Concerns include the impact construction and project operation would have on fish spawning and rearing habitat, and bald eagles. The eagles rely on the salmon that use the Chilkoot Valley in the fall and early winter when they are attracted to late spawning salmon runs. A hydro aquatic studies report prepared by the Shipley Group states that according to the Alaska Department of Fish and Game, 41 percent of the sockeye salmon in the upper Lynn Canal come from the Chilkoot River with 25 percent of those salmon spawning in the Chilkoot River drainage above Chilkoot Lake. The value of the fishery is estimated at more than $1,000,000 annually. AP&T announced in June 2013 that it was putting the project on hold citing difficulty securing funding from the Alaska Energy Authority and the lack of community support. Despite these setbacks AP&T says that it not abandoning pursuing the project. In early September 2013, the Haines Borough announced that it was exploring possibly filing for a preliminary permit now that the project was no longer being pursued by AP&T. The large lake in the background is Chilkoot Lake.
    Connelly Lake, Chilkoot River - 3.jpg
  • A Fairweather Range mountainside appears to be unstable in this photo taken at the Canadian and United States border in Tatshenshini-Alsek Provincial Park. 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 />
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The park was designated a UNESCO World Heritage site in 1994.
    Unstable mountainside.jpg
  • Sunrise on coastal mountains seen from Alaska Airlines flight from Seattle to Juneau in southeast Alaska.
    Coastal mountains sunrise from air 1.jpg
  • Snow-covered Connelly Lake (far left) is a 90-acre alpine lake near Haines, Alaska that drains into the Chilkoot River (right). Connelly Lake is the focus of a proposed $32 million, 12-megawatt hydroelectric project by Alaska Power and Telephone Company (AP&T). AP&T proposes to build a dam at the outlet of Connelly Lake that would create a 160-acre reservoir and a 6,200-foot-long penstock down the side of the mountain where water would be delivered to turbine generators located in a powerhouse near the Chilkoot River into which the lake water would be discharged. Some of the main features of the proposed Connelly Lake project (for example portions of the penstock, the powerhouse, access roads, and the transmission line) would be located in the Alaska Chilkat Bald Eagle Preserve and the Haines State Forest. Concerns include the impact construction and project operation would have on fish spawning and rearing habitat, and bald eagles. The eagles rely on the salmon that use the Chilkoot Valley in the fall and early winter when they are attracted to late spawning salmon runs. A hydro aquatic studies report prepared by the Shipley Group states that according to the Alaska Department of Fish and Game, 41 percent of the sockeye salmon in the upper Lynn Canal come from the Chilkoot River with 25 percent of those salmon spawning in the Chilkoot River drainage above Chilkoot Lake. The value of the fishery is estimated at more than $1,000,000 annually. AP&T announced in June 2013 that it was putting the project on hold citing difficulty securing funding from the Alaska Energy Authority and the lack of community support. Despite these setbacks AP&T says that it not abandoning pursuing the project. In early September 2013, the Haines Borough announced that it was exploring possibly filing for a preliminary permit now that the project was no longer being pursued by AP&T. The large lake in the background is Chilkoot Lake. Beyond Chilkoot Lake is Lutak Inlet of the Lynn Canal.
    Connelly Lake, Chilkoot River - 2.jpg