Cape Alava () is a cape in the Pacific Northwest region of the United States. Located in Clallam County, Washington, the cape is situated within Olympic National Park and the Makah Indian Reservation, and is accessible via a 3-mile boardwalk hike from a ranger station in the park.
Cape Alava Trail was designated a National Recreation Trail in 1981.
Nearby Cape Flattery and Cape Blanco in southern Oregon are also very close longitudinally to being the westernmost points in the contiguous 48 states, which are at and respectively.
The Cape became the western terminus of the newly created Pacific Northwest Trail with the passage of the Omnibus Public Land Management Act of 2009.
The rich mixture is a result of the combined Erosion power of the ocean and relatively recent glacial activity. According to the Washington State Department of Natural Resources, the area's are classified as Unconsolidated Deposition, translating to the geological equivalent of a grab bag. More finely, the deposits are listed as "Quaternary Sediments, Dominantly Moraine, includes alluvium". The Quaternary time period dates to the end of the most recent ice age, roughly 10,000 to 14,000 BCE. A [1] shows the unique nature of such sediments being exposed to the full grinding force of the Pacific Ocean. There are many such areas scattered about the Puget Sound, yet very few areas on the unprotected Washington coast.
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