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The lowlands south of Puget Sound were home to an extensive region of prairies. [4] These ecosystems have since been greatly reduced in size due to the repurposing of these lands for agriculture, grazing, industry, and urban development.
The Puget Sound region is a coastal area of the Pacific Northwest in the U.S. state of Washington, including Puget Sound, the Puget Sound lowlands, and the surrounding region roughly west of the Cascade Range and east of the Olympic Mountains. It is characterized by a complex array of saltwater bays, islands, and peninsulas carved out by ...
Puget Sound Lowlands, Washington, U.S. ... The decline is attributed to various issues, including human population growth, pollution, and climate change. [55]
The Vashon Glaciation is an extension of the Fraser Glaciation in which the Cordilleran Ice Sheet advanced south of the present day Canada–United States border into the Puget Sound region. By following the Fraser Valley, the ice reached the Puget Sound Region using the same pathway that cold arctic air takes during a present-day winter cold snap.
In both cases, the windward slopes facing southwest receive high precipitation and mild, cool temperatures. While the Puget Sound lowlands are known for clouds and rain in the winter, the western slopes of the Cascades receive larger amounts of precipitation, often falling as snow at higher elevations. [21]
Everett generally has an oceanic climate similar to most of the Puget Sound lowlands, with year-round moderate temperatures influenced by marine air masses. The variation of normal weather between seasons is less extreme than inland areas, with dry summers and mild, rainy winters due to the proximity of the Pacific Ocean . [ 181 ]
The local terrain is typical of the Puget Sound lowlands, consisting largely of rolling hills formed from glacial till, occasionally interrupted by flatlands typically found near substantial bodies of water. The largest river is the Sammamish, which connects Lake Sammamish to Lake Washington, and divides the city into northern and southern halves.
Monroe has a general climate similar to most of the Puget Sound lowlands, with dry summers and mild, rainy winters moderated by a marine influence from the Pacific Ocean. [77] The majority of the region's precipitation arrives during the winter and early spring, and Monroe averages 177 days of precipitation per year.