Nehalem Bank (Clatsop County, Oregon)

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Nehalem Bank
The Shale Pile
USA Oregon relief location map.svg
Red pog.svg
Nehalem Bank
Nehalem Bank
Location Pacific Ocean, near Tillamook Head
Coordinates 45°54′00″N124°33′00″W / 45.90000°N 124.55000°W / 45.90000; -124.55000
Type Bar
Ocean/sea sources Pacific
Basin  countriesUnited States
Surface area74.6 square kilometres (28.8 sq mi)
Max. depth160 metres (520 ft)
Islands No islands

Nehalem Bank is a bar, off the coast of Oregon, United States. It also has both rocky reefs and mud habitat, and is just northwest of Garibaldi Reef. [1] [2] [3]

Contents

Nehalem Bank runs between 150 metres (490 ft) and 200 metres (660 ft) deep, having an area of 74.6 square kilometres (28.8 sq mi). [4] It is located off Tillamook Head, hence is off Clatsop County, and is barely south of the mouth of the Columbia River and Astoria Canyon. [5] Nehalem Bank is north of Nehalem Bay.

Nehalem Bank is one of the three major offshore banks of Oregon, the other two being Heceta Bank and Coquille Bank. [6] Nehalem Bank compares in size to Heceta Bank. [7]

Fishing

Nehalem Bank has been trawled, for shrimp. [8]

As of 2020, it is illegal to fish the Nehalem Bank with bottom trawl gear. [9]

Oceanography and Geology

Nehalem Bank has underwater sea stacks and paleoshorelines. There are rocky remnants of former seacliffs which are bored with intertidal pholad clam holes, testifying to what the level of the sea once was. [5]

Methane seeps are found, on Nehalem Bank, also, on Heceta Bank and Coquille Bank. These sites have microbial communities, also known as bacterial mats, in patches close to the sources of methane bubbles. They use methane for their metabolism. Whether the methane could be used the generate power is problematic, introduces many questions. [10]

A north-and northwest-striking geologic fault, the Nehalem Bank Fault, crosses the Nehalem Bank, is estimated to slip 0.5 to 5 millimeters per year. [11] [12] In the forearc of the Cascadia Subduction Zone, this fault underlies the continental shelf. [13]

See also

Related Research Articles

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<span class="mw-page-title-main">Nehalem River</span> River in Oregon, United States

The Nehalem River is a river on the Pacific coast of northwest Oregon in the United States, approximately 119 miles (192 km) long. It drains part of the Northern Oregon Coast Range northwest of Portland, originating on the east side of the mountains and flowing in a loop around the north end of the range near the mouth of the Columbia River. Its watershed of 855 square miles (2,210 km2) includes an important timber-producing region of Oregon that was the site of the Tillamook Burn. In its upper reaches it flows through a long narrow valley of small mountain communities but is unpopulated along most of its lower reaches inland from the coast.

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<span class="mw-page-title-main">Clatsop</span>

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Tillamook Head is a high promontory on the Pacific coast of northwest Oregon in the United States. It is located in west-central Clatsop County, approximately 5 mi (8 km) southwest of Seaside. The promontory forms a steep rocky bluff on the ocean, approximately 1,200 ft high, forested with Sitka spruce. It is located in Ecola State Park.

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<span class="mw-page-title-main">Oregon Islands National Wildlife Refuge</span>

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Stonewall Bank, also, the Stonewall Bank Yelloweye Rockfish Conservation Areas (YRCA) is a bar, loosely southwest of Newport, Oregon, United States. Waldport and Yachats are also near. It is 17 miles (27 km) southwest of Yaquina Bay Light, and 14 miles (23 km) offshore. Running north, Stonewall Bank is 9 miles (14 km) long and 2.5 miles (4.0 km) wide. Locally, Stonewall Bank is known as the Rock Pile, has good fishing for salmon, black rockfish and flatfish.

References

  1. Gockel, Catherine (December 9, 2016). "Oregon Department of Fish and Wildlife" (PDF). Retrieved 2020-12-27.
  2. Gockel, Catherine. "Offshore Seafood Processors in Federal Waters Off the Coast of Washington and Oregon (WAG520000)" (PDF). EPA. Retrieved 2020-12-27.
  3. Hannah, Robert. "Information Reports Number 2014-03" (PDF).
  4. Hannah, Robert. "Effects of trawling for ocean shrimp (Pandalus jordani) on macroinvertebrate abundance and diversity at four sites near Nehalem Bank, Oregon" (PDF).
  5. 1 2 Embley, Bob. "Mapping Ancient Shorelines" . Retrieved 2020-12-26.
  6. Milstein, Michael (March 8, 2008). "Oregon tsunami may turn out bigger than thought" . Retrieved December 28, 2020.
  7. McNeill, Lisa C. (August 2000). "Tectonics of the Neogene Cascadia forearc basin: Investigations of a deformed late Miocene unconformity" (PDF). Retrieved 2020-12-28.
  8. Hannah, Robert. "Fish Division Oregon Department of Fish and Wildlife" (PDF).
  9. Floyd, Mark (June 6, 2018). "Oregon's Methane Coast" . Retrieved 2020-12-26.
  10. "Nehalem Bank fault (Class A) No. 789".
  11. Personius, Stephen F. "Map and data for Quaternary faults and folds in Oregon" (PDF).
  12. Personius, S.F. (May 17, 2002). "Quaternary Fault and Fold Database of the United States" . Retrieved 2020-12-28.

General references

Geologic references