Glacial erratic boulders of Island County, Washington

Locations of glacial erratics in Island County.

Glacial erratic boulders in Island County are a remnant of the Pleistocene glaciation that created Puget Sound and transformed the surfaces of what are now Island County's main landmasses: Whidbey Island and Camano Island. South of Deception Pass, the two islands' surfaces and beaches are completely composed of glacial till.[1][2]:5 Abundant glacial erratic boulders lie on the islands, their beaches, and under the near-shore waters.[3][4]

List of boulders

Big Rock, once known as the Rock of Ages, is a 30-foot (9.1 m) high greenstone erratic and a landmark on Main Street in Coupeville, at one time considered for a city conservation easement.[5][6][7]

48°12′38″N 122°41′14″W / 48.21056°N 122.68722°W / 48.21056; -122.68722 (Big Rock (Coupeville))

Camano Island State Park erratic is on the south cliff trail in Camano Island State Park, overlooking Saratoga Passage.[8]

48°07′43″N 122°29′59″W / 48.12861°N 122.49972°W / 48.12861; -122.49972 (Camano Island State Park erratic)

Chuckanut erratic is a 10-foot (3.0 m) tall Chuckanut Formation sandstone boulder on the beach below Double Bluff.[9]

47°58′30″N 122°31′07″W / 47.97500°N 122.51861°W / 47.97500; -122.51861 (Chuckanut erratic)

The Clinton erratic is a greenstone boulder with north-south glacial striations, at the corner of Conrad St and Berg Road above the ferry terminal in the town of Clinton. The rock and Coupeville's Big Rock were used to calibrate 36Cl radiometric dating due to the well established date they were deposited and began to receive cosmic ray bombardment.[10][11][12]

47°58′23.7″N 122°21′9.36″W / 47.973250°N 122.3526000°W / 47.973250; -122.3526000 (Clinton erratic)

Footprint Rock is a boulder near Smugglers Cove on Whidbey Island's west side. The rock, high in the intertidal zone, gets its name from a "footprint like impression".[4]

48°3′57.96″N 122°36′19.8″W / 48.0661000°N 122.605500°W / 48.0661000; -122.605500 (Footprint Rock)

The Holmes Harbor erratic is on the eastern shore of Holmes Harbor, and is somewhat taller than a man.[13]

48°04′52″N 122°31′01″W / 48.08111°N 122.51694°W / 48.08111; -122.51694 (Holmes Harbor erratic)

Klootchman Rock (also spelled Kloochman) is metamorphic rock boulder with white veins. The 35-foot (11 m)[14] tall boulder topped with grass, and its broken shards sit at the base of Blowers Bluff between Penn Cove and Oak Harbor.[15][16] The rock has a National Geodetic Survey control station at its highest point.[14] There is a submerged feature (bar) also called Klootchman Rock about 100 meters offshore.[17]

48°15′00″N 122°39′14″W / 48.25000°N 122.65389°W / 48.25000; -122.65389

Scatchet Head erratics are on the beach below bluffs at the southwest point of Whidbey Island.[18]

47°54′51.48″N 122°25′52.32″W / 47.9143000°N 122.4312000°W / 47.9143000; -122.4312000 (Scatchet Head)

Waterman Rock is a house-sized greenschist erratic with a circumference of 155 feet (47 m) and height of 38 feet (12 m)[9] to 40 feet (12 m) or greater[19][2]:5 in Saratoga Woods Preserve near Langley.[6][20][21] It may be the second largest erratic in Washington State, after the Lake Stevens Monster.[9] The property including the rock was acquired in 2002[2]:4 or 2005[19] for conservation.

48°03′38″N 122°27′47″W / 48.06056°N 122.46306°W / 48.06056; -122.46306 (Waterman Rock)

References

  1. Tucker 2010a.
  2. 1 2 3 Whidbey Camano Land Trust and Island County (August 2010), Saratoga Management Plan (PDF), Island County Parks
  3. Haugerud 2008.
  4. 1 2 Mary Jo Adams and Judi McD. (March 7, 2008), Intertidal Monitoring - 2007, Coupeville, WA: Washington State University Island County Extension
  5. "UW professor puts Big Rock in its geologic place", South Whidbey Record, June 25, 2008
  6. 1 2 Burnett, Justin (January 4, 2012), "Big Rock for sale: Giant stone goes with Coupeville apartments", Whidbey News-Times, retrieved June 1, 2015
  7. Whalen, Nathan (January 27, 2012), "Coupeville Town Council unmoved by Big Rock", Whidbey News-Times, retrieved June 1, 2015
  8. Tom Barr (July 3, 1991), "Camano Island State Park Offers Wide Choice Of Facilities, Activities", The Seattle Times
  9. 1 2 3 Tucker 2010b.
  10. University of Washington Earth and Space Sciences 2010
  11. Swanson 2009, p. 7.
  12. Terry W Swanson, Marc L Caffee (January 2003), "Determination of 36Cl Production Rates Derived from the Well-Dated Deglaciation Surfaces of Whidbey and Fidalgo Islands, Washington", Quaternary Research 59 (1): 132–134, doi:10.1006/qres.2001.2278
  13. Western Geo Hikes 2008.
  14. 1 2 National Geodetic Survey PID TR1338, "Blowers Bluff Klootchman Rock"
  15. Hugh Shipman (May 9, 2011), "Klootchman Rock", Gravel Beach (blog)
  16. Overton, Harold L. (June 20, 2012), Quadransphere of North America
  17. U.S. Geological Survey Geographic Names Information System: Klootchman Rock
  18. R.C. Ray (1891), The Coast of British Columbia Including The Juan de Fuca Strait, Puget Sound, Vancouver and Queen Charlotte Islands, United States Navy Hydrographic Office/Government Printing Office, p. 29
  19. 1 2 "County sets Southend rockin'", South Whidbey Record, June 25, 2008
  20. Sheets, Bill, "Big boulder in Edmonds one of many left by long-gone glaciers", Everett Herald, retrieved June 1, 2015
  21. Karen Sykes (January 29, 2003), "Hike of the week: Wandering through Whidbey Island woods", The Seattle Times

Sources

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