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  • Aialik Glacier pours down the mountains from the Harding Icefield as seen from the Aialik public use cabin on Aialik Bay in Kenai Fjords National Park in Alaska. 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. SPECIAL NOTE: This image is a panorama composite consisting of multiple overlapping images stitched together.
    Aialik Glacier.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
  • 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
  • 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
  • Deep crevasses of Margerie Glacier take on an other worldly look in early evening light in this photo taken at the uppermost region of the glacier just inside the U.S. at the Canadian border. The 21-mile-long glacier in Glacier Bay National Park and Preserve is one of the park’s tidewater glaciers. <br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Margerie Glacier crevasses-2.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Alaska Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
Mountainsides that were held strong by the heavy ice of glaciers become weak when the glaciers retreat. Erosion along with earthquakes are triggers that can cause the weakened slopes to collapse.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide-6.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Alaska Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
Mountainsides that were held strong by the heavy ice of glaciers become weak when the glaciers retreat. Erosion along with earthquakes are triggers that can cause the weakened slopes to collapse.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide-4.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Alaska Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
Mountainsides that were held strong by the heavy ice of glaciers become weak when the glaciers retreat. Erosion along with earthquakes are triggers that can cause the weakened slopes to collapse.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide-2.jpg
  • 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
  • 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
  • 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 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
  • The face of Margerie Glacier, one of the seven tidewater glaciers in Glacier Bay National Park and Reserve in southeast Alaska, is riddled with cracks and crevices. The Margerie Glacier is located on the Tarr Inlet next to another tidewater glacier, Grand Pacific Glacier. Margerie Glacier's face has a total height of 350 feet, out of which 250 feet is above the water level and 100 feet is beneath the water surface. For comparison purposes the Statue of Liberty is 307 feet tall.. The Margerie Glacier is located on the Tarr Inlet next to another tidewater glacier, Grand Pacific Glacier. Margerie Glacier's one mile wide glacial face has a total height of 350 feet, out of which 250 feet is above the water level and 100 feet is beneath the water surface. For comparison purposes the Statue of Liberty is 307 feet tall. The length of the glacier (2011) is approximately 21 miles.
    Margerie Glacier 4.jpg
  • The face of Margerie Glacier, one of the seven tidewater glaciers in Glacier Bay National Park and Reserve in southeast Alaska, is riddled with cracks and crevices. The Margerie Glacier is located on the Tarr Inlet next to another tidewater glacier, Grand Pacific Glacier. Margerie Glacier's face has a total height of 350 feet, out of which 250 feet is above the water level and 100 feet is beneath the water surface. For comparison purposes the Statue of Liberty is 307 feet tall.. The Margerie Glacier is located on the Tarr Inlet next to another tidewater glacier, Grand Pacific Glacier. Margerie Glacier's one mile wide glacial face has a total height of 350 feet, out of which 250 feet is above the water level and 100 feet is beneath the water surface. For comparison purposes the Statue of Liberty is 307 feet tall. The length of the glacier (2011) is approximately 21 miles.
    Margerie Glacier 1.jpg
  • An unidentified tourist on the daily tour boat, Baranof Wind,admires the face of Margerie Glacier, one of the seven tidewater glaciers in Glacier Bay National Park and Reserve in southeast Alaska. The Margerie Glacier is located on the Tarr Inlet next to another tidewater glacier, Grand Pacific Glacier. Margerie Glacier's one mile wide face has a total height of 350 feet, out of which 250 feet is above the water level and 100 feet is beneath the water surface. For comparison purposes the Statue of Liberty is 307 feet tall. The length of the glacier (2011) is approximately 21 miles. The mountain pictured is Mount Forde.
    Tourist views Margerie Glacier.jpg
  • The face of Margerie Glacier, one of the seven tidewater glaciers in Glacier Bay National Park and Reserve in southeast Alaska, is riddled with cracks and crevices. The Margerie Glacier is located on the Tarr Inlet next to another tidewater glacier, Grand Pacific Glacier. Margerie Glacier's face has a total height of 350 feet, out of which 250 feet is above the water level and 100 feet is beneath the water surface. For comparison purposes the Statue of Liberty is 307 feet tall.. The Margerie Glacier is located on the Tarr Inlet next to another tidewater glacier, Grand Pacific Glacier. Margerie Glacier's one mile wide glacial face has a total height of 350 feet, out of which 250 feet is above the water level and 100 feet is beneath the water surface. For comparison purposes the Statue of Liberty is 307 feet tall. The length of the glacier (2011) is approximately 21 miles.
    Margerie Glacier 3.jpg
  • The face of Margerie Glacier, one of the seven tidewater glaciers in Glacier Bay National Park and Reserve in southeast Alaska, is riddled with cracks and crevices. The Margerie Glacier is located on the Tarr Inlet next to another tidewater glacier, Grand Pacific Glacier. Margerie Glacier's face has a total height of 350 feet, out of which 250 feet is above the water level and 100 feet is beneath the water surface. For comparison purposes the Statue of Liberty is 307 feet tall.. The Margerie Glacier is located on the Tarr Inlet next to another tidewater glacier, Grand Pacific Glacier. Margerie Glacier's one mile wide glacial face has a total height of 350 feet, out of which 250 feet is above the water level and 100 feet is beneath the water surface. For comparison purposes the Statue of Liberty is 307 feet tall. The length of the glacier (2011) is approximately 21 miles.
    Margerie Glacier 2.jpg
  • Icebergs from McBride Glacier pool together in McBride Inlet located just off the Muir Inlet in Glacier Bay National Park and Preserve in southeast Alaska. The McBride Glacier, the most active glacier and only tidewater glacier in the Muir Inlet, is retreating. In 1966 the terminus of the glacier was roughly where the ice in the foreground is. In this 2011 photo the glacier's terminus is approximately 3.5 miles away. The mountain peak in the background is Coleman Peak. McBride Glacier is one of the park's seven tidewater glaciers.
    McBride Glacier.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
  • The face of Margerie Glacier, one of the seven tidewater glaciers in Glacier Bay National Park and Reserve in southeast Alaska, is riddled with cracks and crevices. The Margerie Glacier is located on the Tarr Inlet next to another tidewater glacier, Grand Pacific Glacier. Margerie Glacier's one mile wide face has a total height of 350 feet, out of which 250 feet is above the water level and 100 feet is beneath the water surface. For comparison purposes the Statue of Liberty is 307 feet tall. The length of the glacier (2011) is approximately 21 miles. SPECIAL NOTE: This image is a panorama composite consisting of multiple overlapping images stitched together.
    Margerie Glacier panorama.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
  • Tourists on the daily tour boat, Baranof Wind, photograph the face of Margerie Glacier, one of the seven tidewater glaciers in Glacier Bay National Park and Reserve in southeast Alaska. The Margerie Glacier is located on the Tarr Inlet next to another tidewater glacier, Grand Pacific Glacier. Margerie Glacier's one mile wide face has a total height of 350 feet, out of which 250 feet is above the water level and 100 feet is beneath the water surface. For comparison purposes the Statue of Liberty is 307 feet tall. The length of the glacier (2011) is approximately 21 miles.
    Tourists photograph Margerie Glacier.jpg
  • A portion of the face of Margerie Glacier, one of the seven tidewater glaciers in Glacier Bay National Park and Reserve in southeast Alaska collapses with a loud rifle sounding "crack" and booming roar. The Margerie Glacier is located on the Tarr Inlet next to another tidewater glacier, Grand Pacific Glacier. Margerie Glacier's one mile wide face has a total height of 350 feet, out of which 250 feet is above the water level and 100 feet is beneath the water surface. For comparison purposes the Statue of Liberty is 307 feet tall. The length of the glacier (2011) is approximately 21 miles.
    Margerie Glacier collapse.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 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
  • A meadow of tall fireweed booms in Brotherhood Bridge Park in Juneau, Alaska. In the background is the Mendenhall Glacier, one of the most accessible glaciers in southeast Alaska. Each year, 465,000 curise ship passengers visit the Mendenhall Glacier.
    Tall fireweed and Mendenhall Glacier.jpg
  • 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
  • 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
  • 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-8.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Anchorage Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide-5.jpg
  • A 4,000-foot-high mountainside released approximately 120 million metric tons of rock in 60 seconds during a landslide onto the Lamplugh Glacier in Glacier Bay National Park and Preserve. In an interview with the Anchorage Dispatch News, geophysicist Colin Stark of Columbia University's Lamont-Doherty Earth Observatory, described the slide as “exceptionally large.” He compared the massive landslide to roughly 60 million medium SUVs tumbling down a mountainside.<br />
<br />
The slide occurred on the morning of June 28  in a remote area of Glacier Bay National Park in southeast Alaska. It was first observed by Paul Swanstrom, pilot and owner of Haines-based Mountain Flying Service. Swanstrom noticed a huge cloud of dust over the Lamplugh Glacier during a flightseeing tour of Glacier Bay National Park several hours after the slide occurred. Swanstrom estimates the debris field to be 6.5 miles long, and one to two miles in width.<br />
<br />
Even two days later, as this aerial photo of the Lamplugh Glacier landslide shows, a dust cloud remained over the unstable mountainside due to still tumbling rock.
    Lamplugh Glacier landslide-3.jpg
  • 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 Mendenhall Glacier runs roughly 12 miles, originating in the Juneau Icefield, near Juneau, Alaska. The US Forest Service visitor center at the glacier, dedicated in 1963, was the first such center in the nation. The glacier is located 12 miles from downtown Juneau. Each year, 465,000 curise ship passengers visit the Mendenhall Glacier.
    Mendenhall Glacier-2.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. The mountain ridge in the center is McConnell Ridge.
    McBride Glacier, icebergs aerial.jpg
  • Riggs Glacier is retreating and is no longer considered a tidewater glacier. The glacier located just off the Muir Inlet is located in Glacier Bay National Park and Preserve in southeast Alaska.
    Riggs Glacier panorama.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
  • 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.jpg
  • Icebergs float in Mendenhall Lake located at the terminus of the Mendenhall Glacier. Also pictured in the background is Mount Wrather. The Mendenhall Glacier runs roughly 12 miles, originating in the Juneau Icefield, near Juneau, Alaska. The glacier is located 12 miles from downtown Juneau. Each year, 465,000 curise ship passengers visit the Mendenhall Glacier.
    Glacier reflection.jpg
  • Icebergs reflect in Mendenhall Lake located at the terminus of the Mendenhall Glacier. The Mendenhall Glacier runs roughly 12 miles, originating in the Juneau Icefield, near Juneau, Alaska. The glacier is located 12 miles from downtown Juneau. Each year, 465,000 curise ship passengers visit the Mendenhall Glacier.
    Glacier iceberg reflection.jpg
  • The Saksaia Glacier sits at the top of the Glacier Creek valley near the location of the potential mine site being explored by Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan. The area of exploration, known as the Palmer Deposit is located near mile 40 of the Haines Highway and the Porcupine placer gold mining area near Haines, Alaska.<br />
<br />
The minerals that Constantine’s drilling explorations have found are primarily copper and zinc, with significant amounts of gold and silver. Exploratory drilling to refine the location and mineral amounts are the current focus of the company.<br />
<br />
If approved and developed, the mine would be an underground mine. Besides the actual ore deposits, having the nearby highway access for transporting ore to the deepwater port at Haines is also attractive to Constantine.<br />
<br />
Support for a large scale mine such as the Constantine project is divided among residents of Haines, a small community in Southeast Alaska 75 miles northwest of Juneau. The community’s needed economic boost from jobs, development and other mine support that a large-scale mine brings is tempting to some. To others, anything that might put the salmon spawning and rearing habitat and watershed resources at risk is simply unimaginable and unacceptable. Of particular concern is copper and other heavy metals in mine waste leaching into the Klehini and Chilkat River. Copper and heavy metals are toxic to salmon and bald eagles.<br />
<br />
The Chilkat River chum salmon are the primary food source for one of the largest gatherings of bald eagles in the world. Each fall, bald eagles congregate in the Alaska Chilkat Bald Eagle Preserve, located only three miles downriver from the area of current exploration. At times more than 3,000 eagles have been recorded at the primary gathering area for the fall chum salmon run.
    Saksaia Glacier 3.jpg
  • 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
  • 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
  • The Mendenhall Glacier runs roughly 12 miles, originating in the Juneau Icefield, near Juneau, Alaska. This photo of the glacier was taken on the Trail of Time. The glacier is located 12 miles from downtown Juneau. Each year, 465,000 curise ship passengers visit the Mendenhall Glacier.
    Mendenhall Glacier in the fall.jpg
  • The Mendenhall Glacier runs roughly 12 miles, originating in the Juneau Icefield, near Juneau, Alaska. This photo of the glacier was taken on the Trail of Time. The glacier is located 12 miles from downtown Juneau.
    Mendenhall Glacier in the fall.jpg
  • Icebergs reflect in Mendenhall Lake located at the terminus of the Mendenhall Glacier. The Mendenhall Glacier runs roughly 12 miles, originating in the Juneau Icefield, near Juneau, Alaska. The glacier is located 12 miles from downtown Juneau.
    Glacier iceberg reflection-2.jpg
  • The Saksaia Glacier sits at the top of the Glacier Creek valley near the location of the potential mine site being explored by Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan. The area of exploration, known as the Palmer Deposit is located near mile 40 of the Haines Highway and the Porcupine placer gold mining area near Haines, Alaska.<br />
<br />
The minerals that Constantine’s drilling explorations have found are primarily copper and zinc, with significant amounts of gold and silver. Exploratory drilling to refine the location and mineral amounts are the current focus of the company.<br />
<br />
If approved and developed, the mine would be an underground mine. Besides the actual ore deposits, having the nearby highway access for transporting ore to the deepwater port at Haines is also attractive to Constantine.<br />
<br />
Support for a large scale mine such as the Constantine project is divided among residents of Haines, a small community in Southeast Alaska 75 miles northwest of Juneau. The community’s needed economic boost from jobs, development and other mine support that a large-scale mine brings is tempting to some. To others, anything that might put the salmon spawning and rearing habitat and watershed resources at risk is simply unimaginable and unacceptable. Of particular concern is copper and other heavy metals in mine waste leaching into the Klehini and Chilkat River. Copper and heavy metals are toxic to salmon and bald eagles.<br />
<br />
The Chilkat River chum salmon are the primary food source for one of the largest gatherings of bald eagles in the world. Each fall, bald eagles congregate in the Alaska Chilkat Bald Eagle Preserve, located only three miles downriver from the area of current exploration. At times more than 3,000 eagles have been recorded at the primary gathering area for the fall chum salmon run.
    Saksaia Glacier 1.jpg
  • Eagle Glacier as seen from Favorite Channel just outside Juneau.
    Eagle Glacier-2.jpg
  • Eagle Glacier looms over the light station (lighthouse) at Point Retreat, near Juneau, Alaska.
    Eagle Glacier.jpg
  • Rainbow Glacier as seen from the Lynn Canal near Haines, Alaska.
    Rainbow Glacier.jpg
  • Davidson Glacier is framed by Talsani Island and the tip of the Chilkat Peninsula, in this view from the Lynn Canal near Haines, Alaska.
    Davidson Glacier.jpg
  • The Saksaia Glacier sits at the top of the Glacier Creek valley near the location of the potential mine site being explored by Constantine Metal Resources Ltd. of Vancouver, British Columbia along with investment partner Dowa Metals & Mining Co., Ltd. of Japan. The area of exploration, known as the Palmer Deposit is located near mile 40 of the Haines Highway and the Porcupine placer gold mining area near Haines, Alaska.<br />
<br />
The minerals that Constantine’s drilling explorations have found are primarily copper and zinc, with significant amounts of gold and silver. Exploratory drilling to refine the location and mineral amounts are the current focus of the company.<br />
<br />
If approved and developed, the mine would be an underground mine. Besides the actual ore deposits, having the nearby highway access for transporting ore to the deepwater port at Haines is also attractive to Constantine.<br />
<br />
Support for a large scale mine such as the Constantine project is divided among residents of Haines, a small community in Southeast Alaska 75 miles northwest of Juneau. The community’s needed economic boost from jobs, development and other mine support that a large-scale mine brings is tempting to some. To others, anything that might put the salmon spawning and rearing habitat and watershed resources at risk is simply unimaginable and unacceptable. Of particular concern is copper and other heavy metals in mine waste leaching into the Klehini and Chilkat River. Copper and heavy metals are toxic to salmon and bald eagles.<br />
<br />
The Chilkat River chum salmon are the primary food source for one of the largest gatherings of bald eagles in the world. Each fall, bald eagles congregate in the Alaska Chilkat Bald Eagle Preserve, located only three miles downriver from the area of current exploration. At times more than 3,000 eagles have been recorded at the primary gathering area for the fall chum salmon run.
    Saksaia Glacier 2.jpg
  • A full moon rises above Mount Ernest Gruering and the Herbert Glacier near Juneau, Alaska as the final rays of the sun at sunset baths mountain tops in alpenglow light. The view is from the Alaska Marine Highway System ferry FVF Fairweather as it traveled down the Lynn Canal from Haines.
    Moonrise over Herbert Glacier.jpg
  • The Thorofare River travels past the terminus of the 34-mile Muldrow Glacier near the Thorofare ranger cabin in Denali National Park in Alaska. The glacier has accumulated rocks and dirt in its journey down from the mountains. This moraine material, along with vegetation growing on top, hides the ice under the surface.
    Muldrow glacier.jpg
  • The Thorofare River travels past the terminus of the 34-mile Muldrow Glacier near the Thorofare ranger cabin in Denali National Park in Alaska. The glacier has accumulated rocks and dirt in its journey down from the mountains. This moraine material, along with vegetation growing on top, hides the ice under the surface.
    Muldrow glacier and Thorofare River.jpg
  • A hiker hikes next to the Thorofare River as it travels past the terminus of the 34-mile Muldrow Glacier near the Thorofare ranger cabin in Denali National Park in Alaska. The glacier has accumulated rocks and dirt in its journey down from the mountains. This moraine material, along with vegetation growing on top, hides the ice under the surface.
    Muldrow glacier and Thorofare River-...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 small peak on the slopes of Mount Wrather looks down upon the Mendenhall Glacier. The Mendenhall Glacier runs roughly 12 miles, originating in the Juneau Icefield, near Juneau, Alaska. The glacier is located 12 miles from downtown Juneau. Each year, 465,000 curise ship passengers visit the Mendenhall Glacier.
    Mount Wrather 2.jpg
  • An iceberg floats in Mendenhall Lake located at the terminus of the Mendenhall Glacier. Also reflected in the lake is Bullard Mountain and Nugget Falls. The glacier runs roughly 12 miles, originating in the Juneau Icefield, near Juneau, Alaska. The glacier is located 12 miles from downtown Juneau. Each year, 465,000 curise ship passengers visit the Mendenhall Glacier.
    Bullard Mountain reflection.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
  • Steep Creek begins to freeze  near the Mendenhall Glacier (center). Mountain on the left is McGinnis Mountain. The Mendenhall Glacier runs roughly 12 miles, originating in the Juneau Icefield, near Juneau, Alaska. The glacier is located 12 miles from downtown Juneau.
    Steep Creek.jpg
  • A portion of the Haines State Forest pictured in this photo (hill area in the center) 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 the Baby Brown Timber Sale area near Haines Alaska between Porcupine Creek (left) and Glacier Creek (right). The Klehini River is in the foreground. The photo was taken from the Haines Highway (AK-7). The Baby Brown Timber Sale also includes forest land west of Glacier Creek to Jarvis Creek.<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 (right mountain slope). 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.<br />
<br />
EDITORS NOTE: This panorama image was produced by electronically stitching together multiple single images.
    Baby Brown Timber Sale.jpg
  • The slopes of Mount Wrather tower above the Mendenhall Glacier. The Mendenhall Glacier runs roughly 12 miles, originating in the Juneau Icefield, near Juneau, Alaska. The glacier is located 12 miles from downtown Juneau.
    Mount Wrather.jpg
  • This steel pipe built between 1912 and 1914 once carried water over one mile from Nugget Creek to the Nugget Creek Powerhouse. The pipe is located on the Trail of Time near the Mendenhall Glacier just outside Juneau, Alaska.
    Nugget Creek water pipe.jpg
  • This steel pipe built between 1912 and 1914 once carried water over one mile from Nugget Creek to the Nugget Creek Powerhouse. The pipe is located on the Trail of Time near the Mendenhall Glacier just outside Juneau, Alaska.
    Nugget Creek water pipe
  • Denali (Athabaskan for "The High One") basks in morning light at sunrise in Denali National Park and Preserve in Alaska. The snow and glacier covered mountain, part of the Alaska Range soars to a height of 20,310 feet. Denali is the tallest mountain on the North American continent. Although Mt. Everest is higher, the vertical rise of Denali is greater. This view is a small detail from the north slopes of the mountain seen from Wonder Lake.
    Denali detail.jpg
  • Denali (Athabaskan for "The High One") basks in morning light at sunrise in Denali National Park and Preserve in Alaska. The snow and glacier covered mountain, part of the Alaska Range soars to a height of 20,310 feet. Denali is the tallest mountain on the North American continent. Although Mt. Everest is higher, the vertical rise of Denali is greater. This view is a small detail from the north slopes of the mountain seen from Wonder Lake.
    Denali detail.jpg
  • Grizzly bear and gray wolf tracks are captured in the mud of the Thorofare River near the Thorofare ranger cabin and the terminus of the Muldrow Glacier in Denali National Park and Preserve in Alaska.
    Grizzly bear and wolf tracks.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
  • 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
  • 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
  • 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
  • Fallen debris on the side of a valley of the Johns Hopkins Glacier in Glacier Bay National Park and Preserve appears to be almost feather-like.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. Known for its spectacular tidewater glaciers, icefields, and tall costal mountains, the park is also an important marine wilderness area. The park a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Johns Hopkins Glacier debris.jpg
  • A meadow of tall fireweed booms in Brotherhood Bridge Park in Juneau, Alaska. In the background is the Mendenhall Glacier, one of the most accessible glaciers in southeast Alaska. Each year, 465,000 curise ship passengers visit the Mendenhall Glacier.
    Tall fireweed and Mendenhall Glacier.jpg
  • A meadow of tall fireweed booms in Brotherhood Bridge Park in Juneau, Alaska. In the background is the Mendenhall Glacier, one of the most accessible glaciers in southeast Alaska. Each year, 465,000 curise ship passengers visit the Mendenhall Glacier.
    Tall fireweed and Mendenhall Glacier.jpg
  • 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
  • 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
  • Unnamed mountain peaks near Sinclair Mountain in the Kakuhan Range bask in light from the setting sun in this sunset view seen from the Portage Cove harbor in Haines, Alaska. SPECIAL NOTE: DIGITAL COMPOSITE PANORAMA (multiple overlapping images stitched together)
    Sunset on Kakuhan Range mountain pea...jpg
  • Afternoon sunlight shines on the slopes of Mount Jonathan Ward outside Haines, Alaska near the Alaska Chilkat Bald Eagle Preserve. Mountains in the Haines area are a popular destination for heli-skiing.
    Mount Jonathan Ward.jpg
  • DIGITAL COMPOSITE PANORAMA (multiple overlapping images stitched together): Four Winds Mountain near Haines, Alaska and near the border with Alaska and British Columbia, Canada rises out of low-lying clouds. This view of the mountain is from the Alaska Chilkat Bald Eagle Preserve.
    Four Winds Mountain panorama.jpg
  • Four Winds Mountain near Haines, Alaska and near the border with Alaska and British Columbia, Canada is bathed in afternoon sunlight. This view of the mountain is from the Alaska Chilkat Bald Eagle Preserve. Mountains in the Haines area are a popular destination for heli-skiing.
    Four Winds Mountain.jpg
  • Four Winds Mountain near Haines, Alaska and near the border with Alaska and British Columbia, Canada rises out of low-lying clouds along the Chilkat River in the Alaska Chilkat Bald Eagle Preserve.
    Four Winds Mountain above Chilkat Ri...jpg
  • Four Winds Mountain near Haines, Alaska and near the border with Alaska and British Columbia, Canada is bathed in afternoon sunlight. The mountain can be seen from the Alaska Chilkat Bald Eagle Preserve.
    Four Winds Mountain-3.jpg
  • Four Winds Mountain near Haines, Alaska and near the border with Alaska and British Columbia, Canada are bathed in afternoon sunlight. The mountain can be seen from the Alaska Chilkat Bald Eagle Preserve.
    Four Winds Mountain-2.jpg
  • Four Winds Mountain near Haines, Alaska and near the border with Alaska and British Columbia, Canada rises out of low-lying clouds. This view of the mountain is from the Alaska Chilkat Bald Eagle Preserve. Mountains in the Haines area are a popular destination for heli-skiing.
    Four Winds Mountain in clouds.jpg
  • James Balog (center), an award winning nature and environmental photojournalist, answers questions from photojournalism students in the gallery of the Angus and Betty McDougall Center for Photojournalism Studies at the Missouri School of Journalism in Columbia, Missouri. Balog was at the university to receive a Missouri Honor Medal In recognition of three decades of using the photographic image to help the public understand the impact of environmental change. Balog is the founder and director of the Extreme Ice Survey (EIS) and the Earth Vision Trust.
    James Balog.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 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
  • A kayaker kayaks past a small iceberg floating in the Muir Inlet of Glacier Bay National Park. This piece of glacial ice is technically not an iceberg due to its small size. The size category for an iceberg is huge, with the height of the ice must be greater than 16 feet above sea level, a thickness of 98-164 feet, with a coverage area greater than 5,382 square feet. Next size down is bergy bits (height less than 16 feet above sea level but greater than three feet), then growlers (less than three feet above sea level - the size of a truck or grand piano), and then brash ice.<br />
<br />
The piece of ice is from the retreating McBride Glacier. Recent research determined that there is 11% less glacial ice in Glacier Bay than in the 1950s. Still, even with the earth’s rapidly changing climate, Glacier Bay is home to a few stable glaciers due to heavy snowfall in the nearby Fairweather Mountains. <br />
<br />
Glacier Bay National Park is located in southeast Alaska. The park is also an important marine wilderness area known for its spectacular tidewater glaciers, icefields, and tall coastal mountains. The park, a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales, which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, Steller sea lions, and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Kayaker and iceberg.jpg
  • A kayaker displays a piece of glacial ice found floating in the Muir Inlet of Glacier Bay National Park. The piece of ice is from the retreating McBride Glacier. Recent research determined that there is 11% less glacial ice in Glacier Bay than in the 1950s. Still even with the earth’s rapidly changing climate, Glacier Bay is home to a few stable glaciers due to heavy snowfall in the nearby Fairweather Mountains. <br />
<br />
Glacier Bay National Park is located in southeast Alaska. The park is also an important marine wilderness area known for its spectacular tidewater glaciers, icefields, and tall coastal mountains. The park, a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales, which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, Steller sea lions, and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Glacial ice.jpg
  • The main bay of Glacier Bay National Park and Preserve is vast, stretching 69 miles from its mouth to the furthest extent. It is hard to imagine that the area pictured (a small portion of the bay) was a single large glacier of solid ice only a little over 200 years ago. In the mid-1700s, this view (and quite a bit beyond) would have been covered by a glacier nearly a mile in thickness. Since then, the massive glacier that filled the bay has retreated 69 miles to the heads of various inlets. <br />
<br />
Recent research determined that there is 11% less glacial ice in Glacier Bay  than in the 1950s. Still, even with the earth’s rapidly changing climate, Glacier Bay is home to a few stable glaciers due to heavy snowfall in the nearby Fairweather Mountains. <br />
<br />
The pictured view is of the Beartrack Mountains looking from Tlingit Point on the left to North Marble Island and South Marble Island on the far right.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. The park is also an important marine wilderness area known for its spectacular tidewater glaciers, icefields, and tall coastal mountains. The park, a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales, which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, Steller sea lions, and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.<br />
<br />
EDITOR’S NOTE: The image is a panoramic composite of several overlapping images.
    Beartrack Mountains panorama.jpg
  • A kayaker kayaks past a small iceberg floating in the Muir Inlet of Glacier Bay National Park. This piece of glacial ice is technically not an iceberg due to its small size. The size category for an iceberg is huge, with the height of the ice must be greater than 16 feet above sea level, a thickness of 98-164 feet, with a coverage area greater than 5,382 square feet. Next size down is bergy bits (height less than 16 feet above sea level but greater than three feet), then growlers (less than three feet above sea level - the size of a truck or grand piano), and then brash ice.<br />
<br />
The piece of ice is from the retreating McBride Glacier. Recent research determined that there is 11% less glacial ice in Glacier Bay than in the 1950s. Still, even with the earth’s rapidly changing climate, Glacier Bay is home to a few stable glaciers due to heavy snowfall in the nearby Fairweather Mountains. <br />
<br />
Glacier Bay National Park is located in southeast Alaska. The park is also an important marine wilderness area known for its spectacular tidewater glaciers, icefields, and tall coastal mountains. The park, a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales, which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, Steller sea lions, and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Kayaker and iceberg-2.jpg
  • These interstadial tree stumps in the Muir Inlet of Glacier Bay National Park and Preserve may look unimpressive, but they are important witnesses to the park's glacial history. Glacier Bay National Park in Southeast Alaska is the largest known repository in North America of interstadial wood from the Holocene period, which began about 11,700 years ago and continues today. Interstadial wood is not fossilized; rather, it was frozen and unfrozen when glaciers advanced and receded in the bay. The forest was sheared off when the glacier advanced but left the stumps behind. Scientists can study the rings of these trees for clues to the glacial timeline of the park. Some stumps in the park date to over 9,000 years ago, and twigs date to 13,700 years ago.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. The park is also an important marine wilderness area known for its spectacular tidewater glaciers, icefields, and tall coastal mountains. The park, a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales, which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, Steller sea lions, and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Interstadial tree stumps.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 skull of a sea otter (Enhydra lutris) lies in the moss of an unnamed island in the Beardslee Islands of Glacier Bay National Park and Preserve. Sea otters, a keystone species of the North Pacific, were almost entirely eliminated by commercial fur hunters in the early 1900s. While they received wildlife protection in 1911, it wasn’t until the early 1990s that sea otters were observed to inhabit Glacier Bay for the first time. As the most abundant marine mammal in Glacier Bay, current estimates put the number of sea otters at 8,000. While orcas are the primary predator of adult sea otters, newborns are preyed upon by bald eagles. Sea otters are positively impacting the kelp forests as the otters protect the kelp forests from excessive grazing by the sea otters’ prey.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. The park is also an important marine wilderness area known for its spectacular tidewater glaciers, icefields, and tall coastal mountains. The park, a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, steller's sea lions, and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Sea otter skull.jpg
  • The Tribal House (Xunaa Shuká Hít) on the shores of Bartlett Cover in Glacier Bay National Park and Preserve was completed in 2015. It is an example of the traditional architectural style of Tlingit ancestral clan houses. Glacier Bay was the traditional home of the Huna Tlingit until the 1700s, when a rapidly advancing glacier pushed them out of the bay. The tribal house project was built as a collaboration between the Huna Tlingit and National Park Service. The tribal house is not only used to tell visitors the story of the Huna Tlingit but it is also used a place for tribal members to reconnect with their homeland and to pass on their traditional and ancestral knowledge to clan members.<br />
<br />
Glacier Bay National Park is located in southeast Alaska. The park is also an important marine wilderness area known for its spectacular tidewater glaciers, icefields, and tall coastal mountains. The park, a popular destination for cruise ships, is also known for its sea kayaking and wildlife viewing opportunities. <br />
<br />
Glacier Bay National Park is home to humpback whales, which feed in the park's protected waters during the summer, both black and grizzly bears, moose, wolves, sea otters, harbor seals, Steller sea lions, and numerous species of sea birds. <br />
<br />
The dynamically changing park, known for its large, contiguous, intact ecosystems, is a United Nations biosphere reserve and a UNESCO World Heritage site.
    Tribal House.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
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