Frozen Marymere Falls

by Inge Johnsson

Title

Frozen Marymere Falls

Artist

Inge Johnsson

Medium

Photograph - Digital Capture, Watermark Not On Actual Print

Description

Marymere Falls, in Washington's Olympic National Park, covered in snow and ice during winter
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Captured with a Canon 5D Mk II and a Canon EF 28-70/2.8L lens
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Marymere Falls is located in Olympic National Park near Lake Crescent in Washington, United States. The falls are accessed by a one-mile, well maintained, dirt trail through old-growth lowland forest consisting of fir, cedar, hemlock, and alder trees. Falls creek descends from Aurora Ridge and tumbles over Marymere Falls and then flows into Barnes Creek. It has a height of 90 feet. The falls is one of the more popular attractions in the area, due to ease of access and proximity to U.S. Highway 101.
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Olympic National Park is located in the U.S. state of Washington, in the Olympic Peninsula. The park can be divided into four basic regions: the Pacific coastline, alpine areas, the west side temperate rainforest and the forests of the drier east side. U.S. President Theodore Roosevelt originally created Mount Olympus National Monument in 1909 and after Congress voted to authorize a re-designation to National Park status, President Franklin Roosevelt signed the legislation June 29, 1938. In 1976, Olympic National Park became an International Biosphere Reserve, and in 1981 it was designated a World Heritage Site. In 1988, Congress designated 95 percent of the park as the Olympic Wilderness.
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The western side of the park is mantled by a temperate rain forest, including the Hoh Rain Forest and Quinault Rain Forest, which receive annual precipitation of about 150 inches (380 cm), making this perhaps the wettest area in the continental United States (the island of Kauai in the state of Hawaii gets more rain). As opposed to tropical rainforests and most other temperate rainforest regions, the rainforests of the Pacific Northwest are dominated by coniferous trees, including Sitka Spruce, Western Hemlock, Coast Douglas-fir and Western redcedar. Mosses coat the bark of these trees and even drip down from their branches in green, moist tendrils. Valleys on the eastern side of the park also have notable old-growth forest, but the climate is notably drier. Sitka Spruce is absent, trees on average are somewhat smaller, and undergrowth is generally less dense and different in character. Immediately northeast of the park is a rather small rainshadow area where annual precipitation averages about 16 inches.

Uploaded

February 3rd, 2013

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