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Kenai River bank. The Kenai River [Kee-nye] is a meltwater river that drains the central Kenai Peninsula region. Its source is the Kenai Lake. [2] Near Cooper Landing, the lake narrows to form the river. About 12 miles (19 km) from the lake, the river passes through Kenai Canyon for about 2 miles (3.2 km) of fast-flowing whitewater rapids.
The watershed covers about 100,000 km 2 (39,000 sq mi) of southern Alaska, east of the Aleutian Range, south and east of the Alaska Range, receiving water from its tributaries, which include the Knik River, the Little Susitna River, the Susitna and Matanuska rivers, Eagle River, Ship Creek, Resurrection Creek, Portage Creek, Kenai River, and ...
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 (1,046.9 sq mi; 2,711.3 km 2 ) [ 1 ] on the Kenai Peninsula in south-central Alaska , west of the town of Seward .
Sep. 15—The Kenai Peninsula Borough issued an emergency declaration Thursday to ask for state assistance in recovering from ongoing flooding that has damaged homes and roads near the Kenai River.
The Chugach National Forest is a 6,908,540-acre (27,958 km 2) [2] United States National Forest in south central Alaska.Covering portions of Prince William Sound, the Kenai Peninsula and the Copper River Delta, it was formed in 1907 from part of a larger forest reserve.
Sep. 15—The Kenai Peninsula Borough issued an emergency declaration Thursday to ask for state assistance in recovering from ongoing flooding that has damaged homes and roads near the Kenai River.
Hidden Lake is a lake on the Kenai Peninsula of Alaska, formed by an ancient channel of the Kenai River. [ 1 ] [ 2 ] It is located entirely inside the Kenai National Wildlife Refuge . The lake is deepest at its southeast end, with depths up to 148 feet (45 m).
The whole rock succession is closely folded, and the arkoses as well as the slates show cleavage, which is, however, much more perfectly developed in the slates. Immense deposits of gravel occur at a number of localities, but are especially noticeable in the valleys of Sixmile Creek, Resurrection Creek, and Kenai River.