| Nehalem Bank | |
| Other Name: | The Shale Pile |
| Location: | Pacific Ocean, near Tillamook Head |
| Coordinates: | 45.9°N -124.55°W |
| Type: | Bar |
| Oceans: | Pacific |
| Basin Countries: | United States |
| Area: | 74.6km2 |
| Max-Depth: | 160m (530feet) |
| Islands: | No islands |
| Pushpin Map: | Oregon |
| Pushpin Map Alt: | Nehaalem Bank is located off the Oregon coast in the Pacific Ocean |
| Pushpin Map Caption: | Nehalem Bank |
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]
Nehalem Bank runs between 150m (490feet) and 200m (700feet) deep, having an area of 74.6km2.[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]
Nehalem Bank has been trawled, for shrimp.[8]
As of 2020, it is illegal to fish the Nehalem Bank with bottom trawl gear.[9]
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]