The Kenai Peninsula is a large peninsula jutting from the coast of Southcentral Alaska. The name Kenai is derived from the word "Kenaitze" or "Kenaitze Indian Tribe", the name of the Native Athabascan Alaskan tribe, the Kahtnuht’ana Dena’ina, who historically inhabited the area. They called the Kenai Peninsula Yaghanen.
Kenai Fjords National Park is a national park of the United States that comprises the Harding Icefield, its outflowing glaciers, and coastal fjords and islands. The park covers an area of 669,984 acres on the Kenai Peninsula in south-central Alaska, west of the town of Seward.
The Kenai Mountains are a mountain range in the U.S. state of Alaska. They extend 192 km (120 mi) northeast from the southern end of the Kenai Peninsula to the Chugach Mountains, and have an average elevation of 3,000 to 5,000 feet.
An ice field is a mass of interconnected valley glaciers on a mountain mass with protruding rock ridges or summits. They are often found in the colder climates and higher altitudes of the world where there is sufficient precipitation for them to form. The higher peaks of the underlying mountain rock that protrude through the icefields are known as nunataks. Ice fields are larger than alpine glaciers, but smaller than ice caps and ice sheets. The topography of ice fields is determined by the shape of the surrounding landforms, while ice caps have their own forms overriding underlying shapes.
Chenega Glacier is a tidewater glacier located in Prince William Sound and on the Kenai Peninsula in the U.S. state of Alaska.
The Tustumena Glacier is a glacier located on the Kenai Peninsula of Alaska. The Tustumena Glacier begins in the Harding Icefield and makes its way down west for about 20 miles (32 km) until its terminus roughly 5 miles (8.0 km) before Tustumena Lake. The glacier is retreating due to global warming.
The Athabasca Glacier is one of the six principal 'toes' of the Columbia Icefield, located in the Canadian Rockies. The glacier currently loses depth at a rate of about 5 metres (16 ft) per year and has receded more than 1.5 km (0.93 mi) and lost over half of its volume in the past 125 years. Easily accessible, it is the most visited glacier in North America. The leading edge of the glacier is within easy walking distance; however, travel onto the glacier is not recommended unless properly equipped. Hidden crevasses have led to the deaths of unprepared tourists.
Bow Glacier is located in Banff National Park, Alberta, Canada, approximately 37 km (23 mi) northwest of Lake Louise. It can be viewed from the Icefields Parkway. Bow Glacier is an outflow glacier from the Wapta Icefield, which rests along the Continental Divide. Runoff from the glacier supplies water to Bow Lake and the Bow River. The glacier is credited for creating the Bow Valley before retreating at the end of the last glacial maximum.
Crowfoot Glacier is located in Banff National Park, Alberta, Canada, 32 km (20 mi) northwest of Lake Louise, and can be viewed from the Icefields Parkway. The glacier is situated on the northeastern flank of Crowfoot Mountain.
The Sargent Icefield is a large icefield located on the eastern portion of the Kenai Peninsula bordering Prince William Sound in Alaska. The ice field has numerous outflow glaciers including the Chenega, Princeton, and Ellsworth Glaciers.
The Harding Icefield is an expansive icefield located in the Kenai Mountains of the Kenai Peninsula in Alaska. It is also partially located in Kenai Fjords National Park. It is named for U.S. President Warren G. Harding.
Exit Glacier is a glacier derived from the Harding Icefield in the Kenai Mountains of Alaska and one of Kenai Fjords National Park's major attractions. It is one of the most accessible valley glaciers in Alaska and is a visible indicator of glacial recession due to climate change. Exit Glacier retreated approximately 187 feet (57 m) from 2013 to 2014 and park scientists continue to monitor and record the glacier's accelerating recession.
The Princeton Glacier is a glacier in the Sargent Icefield, Kenai Peninsula in Alaska.
The Misty Icefield is a high glaciated plateau in the Garibaldi Ranges of the Pacific Ranges of the Coast Mountains. It is located in the eastern part of Garibaldi Provincial Park and the northern portion of Golden Ears Provincial Park. The Misty Icefield was mapped and named in 1955, and rarely visited since, mainly due to its remote location. The area includes the Stave Glacier, and the Snowcap Glacier
The Cambria Icefield is an icefield in the Boundary Ranges of the Coast Mountains in northwestern British Columbia, Canada, located southeast of Stewart.
The Aialik Glacier is a glacier in the Kenai Peninsula Borough of Alaska. It drains into Aialik Bay. Part of Kenai Fjords National Park, it drains the Harding Icefield. Aialik Glacier, a little over 15 miles from Seward, is the largest glacier in Aialik Bay, located in Kenai Fjords National Park. While fairly stable, the glacier calves most actively in May and June.
Holgate Glacier is a glacier located in the U.S. state of Alaska, in Kenai Fjords National Park. It flows outward from the Harding Icefield toward Holgate Arm of Aialik Bay. Tour boats from Seward, Alaska offer tourists the opportunity to view the glacier.
Bear Mountain is a 4,019-foot (1,225 m) mountain summit located in the Kenai Mountains, on the Kenai Peninsula, in the U.S. state of Alaska. The peak is situated in Chugach National Forest, 5 mi (8 km) northeast of Bear Glacier, 2.1 mi (3 km) south-southeast of Marathon Mountain, and 5 mi (8 km) southwest of Seward, Alaska. The peak's local name was reported in 1951 by the U.S. Geological Survey. The months May and June offer the most favorable weather for viewing the mountain. In fair weather, the Harding Icefield can be seen from the summit.
Truuli Peak is a mountain summit located in the Kenai Mountains, in the U.S. state of Alaska. At 6,612 ft, Truuli Peak is the highest mountain in the Kenai Mountains on the Kenai Peninsula in southern Alaska. It is located in the Kenai National Wildlife Refuge in the southwest of the Harding Icefield between the Chernof and Truuli glaciers.
