Semiahmoo Spit

age

Archeological evidence indicated the spit has developed across Drayton Harbor over the last 4000 to 5000 years (Grabert & Schwartz, 1972).

description

At the northern most reach of Whatcom County’s shoreline is a spit approximately 2000 meters long trending northeasterly from the north side of Birch Point (fig.2.). The spit separates Drayton Harbor from Semiahmoo Bay and provides some protection for small boats and shoreline developments within the bay.

down the Pacific Northwest coast

Birch Point

elevation

Semiahmoo Spit is a low depositional feature rising approximately two meters above mean high water. Its low undulating sandy surface is covered with beach and grass scattered trees.

growth

The northeasterly growth of Semiahmoo Spit indicates that sediment eroded from Birch Point has been transported by littoral drift northward, leading to the growth of the spit.

map

Whatcom County Shorelines (figure 1)

random

An escalator can never break, it can only become stairs. You would never see an “Escalator Temporarily Out Of Order” sign, just “Escalator Temporarily Stairs”. Sorry for the convenience. We apologize for the fact that you can still get up there. Mitch Hedberg, Just for Laughs, 1998

spit of

Whatcom County, Washington

tags

width

It [Semiahmoo Spit] is only thirty to forty meters wide along its southern connection with Birch Point. High storm waves frequently overtop this area limiting access to the spit. Toward the northeastern end, the spit gently broadens to nearly three hundred meters, and appears to be quite stable.

Wikidata

https://www.wikidata.org/wiki/Q7449352

Wikipedia

Semiahmoo Spit (Wikipedia) Semiahmoo Spit is a spit that protrudes from the westernmost expanse of shore on Semiahmoo Peninsula between Semiahmoo Bay and Drayton Harbor off the coast of Blaine in Whatcom County, Washington state. The spit is home to Semiahmoo Park.