Eek River, Kuskokwim Delta

See more pictures of Eek River here

The Eek River flows northwest for 108 miles (174 km) before joining the Eenayarak River to form Eek Channel in the Yukon-Kuskokwim Delta about 45 miles (72 km) southwest of Bethel, Alaska. The Yup’ik Eskimo name was first reported as "Ik" by Lieutenant Sarichev of the Imperial Russian Navy in 1826 and has been spelled "Eek" on U.S. Coast and Geodetic Survey charts since 1880.

The community of Eek is on the south bank of the Eek River, 12 miles (19 km) east of the Kuskokwim River mouth. It is 35 miles (56 km) south of Bethel and 420 miles (677 km) west of Anchorage. The community was originally located on Eek Channel at the mouth of Apokok Slough and moved to its present location in the 1930s. The Yup'ik name for the village is Ekvicuaq meaning “a small cliff”, possibly referring to the cliff just upriver from the community. The name "Eek" is taken from the river and means “our eyes” and probably refers to the fall flood tide when the water in the Eek River reaches the top of the north riverbank and is said to be reaching the "eyes" of the riverbank.

A town dock and boat launch is on the Eek River that connects to the Kuskokwim River, providing access to most surrounding villages by boat. During winter months many residents utilize travel by snow machine and trails are laid out between the villages in the area. Trails from Eek run to Quinhagak to the south, Tuntutuliak to the west and the Bethel area to the north. Read more here and here. Download the latest version of the CoastView app and explore more of the Eek River here:

Elwha River, Angeles Point

See more pictures of Elwha River here:

The Elwha River flows generally north for 45 miles (72 km) from the Olympic Mountains to the Strait of Juan de Fuca on the Olympic Peninsula, Washington. Most of the river's course is within Olympic National Park. The river source is the Elwha Snowfinger, a perennial snow field located near Dodwell Rixon Pass, at an elevation of 4,763 feet (1,452 m), separating the watersheds of the Elwha and Queets rivers. This snowfield is created by nearly continuous winter and spring avalanches.

The Elwha is one of several rivers in the Pacific Northwest that supports all five species of Pacific salmon (chinook, coho, chum, sockeye, and pink), plus four anadromous trout species (steelhead, coastal cutthroat, bull trout, and Dolly Varden char). From 1911 to 2014, two dams blocked fish passage on the Elwha River. Before the dams were built in 1911, approximately 400,000 adult salmon returned annually to spawn in 70 miles (110 km) of river habitat. By 2014, fewer than 4,000 salmon returned each year in only 4.9 miles (7.9 km) of remaining spawning habitat. The National Park Service removed the two dams as part of the $325 million Elwha Ecosystem Restoration Project. Removal of the Elwha Dam began in September 2011 and was finished in spring 2012, and removal of the Glines Canyon Dam was completed on August 26, 2014. The resulting sediment release created 70 acres (28 ha) of estuary habitat at the Strait of Juan de Fuca.

While the dams had a major impact on the Elwha River, the health of the lower floodplain has been significantly degraded by other human activities. Restoration activities also include removing abandoned dikes and constructing engineered logjams that will allow the river to form side channels and reconnect to its floodplain. The lower floodplain is also being reforested with native species and eradicating exotic plants. Additional actions have been identified in the middle and lower portions of the river as well as in the estuary and nearshore habitat that will further speed complete watershed recovery. Read more here and here. Download the latest version of the CoastView app and explore more of the Elwha River here:

web counter code