The Pacific Mountain Ranges are a series of mountain ranges that run parallel to the Pacific coast of North America. This includes ranges in Alaska, British Columbia, Washington, Oregon, California and Baja California. Some of the most prominent ranges include the Coast Range, Cascade Range, Sierra Nevada, Transverse Ranges and Peninsular Ranges.
These mountain ranges are a result of tectonic activity associated with the subduction of the Pacific Plate beneath the North American Plate. The collision of these two plates has created a complex series of faults and folds that have uplifted and deformed the landscape. The Pacific ranges are characterized by towering peaks, deep valleys, glaciers, and volcanoes.
The range is home to a variety of flora and fauna, including dense forests, grasslands, alpine meadows, and numerous rivers and lakes that support a diverse array of aquatic life. These mountain ranges also play a critical role in the water cycle, as they store and release vast amounts of water through snow melt and precipitation.
The Pacific Mountain Ranges have a significant impact on the climate of the region, as they act as a barrier to prevailing winds, causing a stark difference between the wetter west coast and the drier east. These ranges also contribute to extreme weather events such as heavy rainfall, landslides and floods.
Overall, the Pacific Mountain Ranges are a critical natural feature of the North American landscape, providing important ecological services and serving as a vital economic resource for the communities that call them home.
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