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Humboldt Bay

Bay on the North Coast of California

  • 19 min read
  • 9 chapters
Aerial view of Humboldt Bay and the city of Eureka in Humboldt County, California, USA. View is to the northeast.
Robert Campbell · CC BY-SA 3.0

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Through Body of water, Harbor and Logging

The Port of Humboldt Bay (also referred to as the Port of Eureka) is a deep water port with harbor facilities, including large industrial docks at Fairhaven, Samoa, and Fields Landing designed to serve cargo and other vessels. Several marinas also located in Greater Eureka have the capacity to serve hundreds of small to mid-size boats and pleasure craft. Beginning in the 1850s, the bay was used extensively to export logs and forest products as part of the historic West coast lumber trade, but with the decline of the industry lumber now is only infrequently shipped from the port.

Geography

Humboldt Bay is the only deep-water bay between the San Francisco Bay and Coos Bay, Oregon. The Port of Humboldt Bay is the only port in the region that is dredged regularly to accommodate large ocean-going vessels. Despite being the only protected harbor along nearly 500 miles (800 km) of coastline, the bay's location was undiscovered for centuries after the first arrival of European explorers. This is partially because the bay is difficult to see from the ocean. The harbor opens to the sea through a narrow and historically treacherous passage, which was blocked from direct view because of sandbars. Formation of such sandbars is now managed by a system of jetties. Contributing to the bay's isolation were features of the coastal mountain range, which extends from the ocean approximately 150 miles (240 km) inland, and the common marine layer (fog) in addition to frequent clouds or rain.

The bay is approximately 14 miles (23 km) long but can be from 0.5 miles (0.80 km) wide at the entrance to the widest point at 4.3 miles (6.9 km) in the North Bay. The surface area of Humboldt Bay is 16,000 acres (65 km2) of which 6,000 acres (24 km2) are intertidal mudflats. More than 5,000 acres (20 km2) are primarily eelgrass habitat, which has been relatively constant since 1871, although more than 80% of the bay's coastal marsh habitats have been lost or fragmented by levee, railroad and highway construction. At high tide the surface area is approximately 24 square miles (62 km2), but it is 10.8 square miles (28 km2) at low tide. Each tidal cycle replaces 41% of the water in Humboldt Bay, although exchange in small channels and sloughs of the bay can take up to three weeks.

Geomorphology

Humboldt Bay began to form when a river valley drowned about 10,000 to 15,000 years ago during a period of rapid sea level rise. Bay sediments also contain buried salt marsh deposits showing that areas of the bay have subsided during episodic large-magnitude subduction earthquakes.

Three rivers, the Mad, Elk, and Eel, drained into Humboldt Bay during the mid-Pleistocene. Subsequently, the Mad River cut a new outlet to the sea, and the flow of the Eel was diverted by tectonic uplift of Table Bluff at the southern end of the bay, but Elk River continues to drain into Humboldt Bay.

In the 21st century, the bay is considered to have three regions:

  • the North Bay to the north of Samoa Bridge
  • the Entrance Bay from Samoa Bridge to South Jetty
  • the South Bay, which is the remainder of the bay to the south

Daby, Woodley, and Tuluwat (formerly Indian) islands are in the North Bay, and all three are within the City of Eureka. Low tides reveal two more islands: Sand Island, which was formed from dredge spoils left in the early 20th century, and Bird Island. A large eelgrass bed in the South Bay, which may be exposed at low tides, is locally known as Clam Island.

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