Orca Inlet lies south and east of Hawkins Island at . The Inlet is about 16 miles (26 km) long running southwest and about 3 miles (4.8 km) wide at its widest point. The south end opens into the Gulf of Alaska while the north end joins with Orca Bay.
The city of Cordova, Alaska is situated on the southeast shore of Orca Inlet.
Orca Inlet was listed in the Geographic Dictionary of Alaska in 1906, citing J.F. Moser's report from 1897. The Orca Cannery operated on the south shore of the inlet; there was a post office at that location from 1894. The Odiak Cannery was located 3 miles southwest of Orca, at the present location of Cordova.
There were once large Razor Clam beds in the intertidal zones of Orca Inlet which were harvested and shipped out of Cordova. Harvests reached 3.5 million pounds at its peak. Populations began to decline in the late 1950s. When the 1964 Good Friday Earthquake struck the clam beds were uplifted around 6 feet (1.8 m) exposing them out of the intertidal zone. This led to moderate mortality and eventually the industry crashed.
Geology and currents
Like other arms of Prince William Sound, Orca Inlet is a fjord. There are large areas on its coast with large rounded rocks as well as many cirques and hanging valleys. Glacial erosion created steep walls on the sides of the fjord. In one area the elevation rises to 1,600 feet (490 m) within 1⁄2 mile (0.80 km) of the coastline. The southern and central areas are filled with sediment making the area very shallow. These deposits resulted from the receded glacier that once filled the fjord as well as current inflow through the seaward end of the inlet from the Copper River and other smaller glacial streams. These deposits drift westward along the coast until they reach the entrance of Orca Inlet. Orca Inlet can serve as an entrance to Prince William Sound from the Gulf of Alaska but the shallow water limits the size of vessels that can use the route. In 1914, the southern 2⁄3rds of the inlet was generally 12 feet (3.7 m) deep or less with a few, discontinuous channels, while the north part was 90 to 228 feet (27 to 69 m) deep.
The tidal current flows southward on the flood and northward on the ebb. Mean velocity at the peak of the flood is 1.5 knots (2.8 km/h; 1.7 mph) and 0.8 knots (1.5 km/h; 0.92 mph) at the peak of the ebb.
- Orca Bay, on the north west side of Hawkins Island
- "Orca Inlet". Geographic Names Information System. U.S. Geological Survey. Retrieved 2010-05-12.
- Ralph Stockman Tarr (1914), Alaskan glacier studies of the National Geographic Society in the Yakutat Bay, Prince William Sound and lower Copper River regions, The National Geographic Society, pp. 385–388
- Baker, Marcus (1906), Geographic dictionary of Alaska (2 ed.), Govt. Print. Off.
- Bishop, Mary Anne; Powers, Sean (2003). "Restoration of Razor Clam (Siliqua patula) Populations in Southeastern Prince William Sound, Alaska". Retrieved May 13, 2010.
- Geological Survey U S (1910), Bulletin - United States Geological Survey, Issue 443, The Survey., p. 70
- U. S. Coast And Geodetic Survey (1916), United States coast pilot: Alaska. Yakutat Bay to Arctic Ocean, Part 2, reprinted by BiblioBazaar, 2009, p. 43