Puget Sound

Coordinates: 47°36′N 122°27′W / 47.6°N 122.45°W / 47.6; -122.45
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Puget Sound

Puget Sound (Template:Pron-en) is a sound in the U.S. state of Washington and Canada Province of British Columbia. It is a complex estuarine system of interconnected marine waterways and basins, with one major and one minor connection to the Strait of Juan de Fuca and the Pacific Ocean—Admiralty Inlet being the major connection and Deception Pass being the minor. Flow through Deception Pass accounts for about 2% of the total tidal exchange between Puget Sound and the Strait of Juan de Fuca.[1] Puget Sound extends approximately 100 miles (160 km) from Deception Pass in the north to Olympia, Washington in the south. Its average depth is 205 feet (62 m) and its maximum depth, off Point Jefferson between Indianola and Kingston, is 930 feet (280 m).[1]

The term "Puget Sound" is used not just for the body of water but also the general region centered on the sound, including the Seattle metropolitan area, home to about 4.4 million people.

Name and definition

There are various definitions of the extent and boundaries of Puget Sound.

In 1792 George Vancouver gave the name "Puget's Sound" to the waters south of the Tacoma Narrows, in honor of Peter Puget, a lieutenant accompanying him on the Vancouver Expedition. The name later came to be used for the waters north of Tacoma Narrows as well.[2]

The USGS defines Puget Sound as all the waters south of three entrances — the main entrance at Admiralty Inlet being a line between Point Wilson, on the Olympic Peninsula, and Point Partridge, on Whidbey Island; a second entrance at Deception Pass being a line from West Point, on Whidbey Island, to Deception Island and Rosario Head, on Fidalgo Island; and a third entrance at the south end of the Swinomish Channel, which connects Skagit Bay and Padilla Bay.[3] Under this definition, Puget Sound includes the waters of Hood Canal, Admiralty Inlet, Possession Sound, Saratoga Passage, and others. It does not include Bellingham Bay, Padilla Bay, the waters of the San Juan Islands or anything farther north.

Another definition, given by NOAA, subdivides Puget Sound into five basins or regions. Four of these correspond to areas within the USGS definition, but the fifth one, called "Northern Puget Sound" includes a large additional region. It is defined as bounded to the north by the international boundary with Canada, and to the west by a line running north from the mouth of the Sekiu River on the Olympic Peninsula.[4] Under this definition significant parts of the Strait of Juan de Fuca and the Strait of Georgia are included in Puget Sound, with the international boundary marking an abrupt and hydrologically arbitrary limit.

According to Arthur Kruckeberg, the term "Puget Sound" is sometimes used for waters north of Admiralty Inlet and Deception Pass, especially for areas along the north coast of Washington and the San Juan Islands, essentially equivalent to NOAA's "Northern Puget Sound" subdivision described above. Kruckeberg uses the term "Puget Sound and adjacent waters".[5]

An alternative term for Puget Sound, still used by only some Native Americans and environmental groups, is Whulge (or Whulj), an Anglicization of the Lushootseed name 'WulcH, which means "Salt Water".[6] Since 2009 the term Salish Sea has been established by the United States Board on Geographic Names as the collective waters of Puget Sound, the Strait of Juan de Fuca, and the Strait of Georgia. Sometimes the terms "Puget Sound" and "Puget Sound and adjacent waters" are used for not only Puget Sound proper but also for waters to the north, such as Bellingham Bay and the San Juan Islands region.[5]

History

See also: Puget Sound region

.

Evening on Puget Sound by Edward S. Curtis, 1913

George Vancouver explored Puget Sound in 1792. Vancouver claimed it for Great Britain on 4 June 1792, naming it for one of his officers, Lieutenant Peter Puget. It was originally administered from Fort Vancouver as part of the Hudson's Bay Company's Columbia Department, but became U.S. territory when the 1846 Oregon Treaty was signed.

The first European settlement in the Puget Sound area was that of Fort Nisqually, in 1833, a farm and trading post of the British Puget Sound Agricultural Company a subsidiary of the Hudson's Bay Company.

After arriving along the Oregon Trail, many settlers wandered north to what is now Washington State and settled the Puget Sound area. The first American settlement was New Market (now known as Tumwater) in 1846. In 1853 Washington Territory was formed from part of Oregon Territory. In 1888 the Northern Pacific railroad line reached Puget Sound, linking the region to eastern states.

Hydrology

Low Tide Whidbey Island

The United States Geological Survey (USGS) defines Puget Sound as a bay with numerous channels and branches; more specifically, it is a fjord system of flooded glacial valleys. Puget Sound is part of a larger physiographical structure termed the Puget Trough, which is a physiographic section of the larger Pacific Border province, which in turn is part of the larger Pacific Mountain System.[7]

Puget Sound is a large salt water estuary, or system of many estuaries, fed by highly seasonal freshwater from the Olympic and Cascade Mountain watersheds. The mean annual river discharge into Puget Sound is 41,000 cubic feet per second (1,200 m3/s), with a monthly average maximum of about 367,000 cubic feet per second (10,400 m3/s) and minimum of about 14,000 cubic feet per second (400 m3/s). Puget Sound's shoreline is 1,332 miles (2,144 km) long, encompassing a water area of 1,020 square miles (2,600 km2) and a total volume of 26.5 cubic miles (110 km3) at mean high water. The average volume of water flowing in and out of Puget Sound during each tide is 1.26 cubic miles (5.3 km3). The maximum tidal currents, in the range of 9 to 10 knots, occurs at Deception Pass.[1]

The Puget Sound system consists of four deep basins connected by shallower sills. The four basins are Hood Canal, west of the Kitsap Peninsula, Whidbey Basin, east of Whidbey Island, South Sound, south of the Tacoma Narrows, and the Main Basin, which is further subdivided into Admiralty Inlet and the Central Basin.[8] Puget Sound's sills, a kind of submarine terminal moraine, separate the basins from one another, and Puget Sound from the Strait of Juan de Fuca. Three sills are particularly significant—the one at Admiralty Inlet which checks the flow of water between the Strait of Juan de Fuca and Puget sound, the one at the entrance to Hood Canal (about 175 ft (53 m)* below the surface), and the one at the Tacoma Narrows (about 145 ft (44 m)*). Other sills that present less of a barrier include the ones at Blake Island, Agate Pass, Rich Passage, and Hammersley Inlet.[5]

Tides in Puget Sound are of the mixed type with two high and two low tides each tidal day. These are called Higher High Water (HHW), Lower Low Water (LLW), Lower High Water (LHW), and Higher Low Water (HLW). The configuration of basins, sills, and interconnections cause the tidal range to increase within Puget Sound. The difference in height between the Higher High Water and the Lower Low Water averages about 0.3 feet (0.091 m) at Port Townsend on Admiralty Inlet, but increases to about 14.4 feet (4.4 m) at Olympia, the southern end of Puget Sound.[1]

Puget Sound is generally accepted as the start of the Inside Passage.[9][10]

Geology

Snowcapped peaks are a backdrop to many Puget Sound scenes; here Mount Rainier is seen from Gig Harbor.

Continental ice sheets have repeatedly advanced and retreated from the Puget Sound region. The most recent glacial period, called the Fraser Glaciation, had three phases, or stades. During the third, or Vashon Glaciation, a lobe of the Cordilleran Ice Sheet, called the Puget Lobe, spread south about 15,000 years ago, covering the Puget Sound region with an ice sheet about 3,000 feet (910 m) thick near Seattle, and nearly 6,000 feet (1,800 m) at the present Canada-US border. Since each new advance of ice scours away much of the evidence of previous ice ages, the most recent Vashon phase has left the clearest imprint on the land. At its maximum extent the Vashon ice sheet extended south of Olympia to near Tenino, and covered the lowlands between the Olympic and Cascade mountains. About 14,000 years ago the ice began to retreat. By 11,000 years ago it survived only north of the Canadian border.[11]

The Vashon Glaciation scoured the land, creating a drumlin field of hundreds of aligned drumlin hills. Lake Washington and Lake Sammamish (which are ribbon lakes), Hood Canal, and the main Puget Sound basin were carved out by glacial forces. As the ice retreated, vast amounts of glacial till were deposited throughout the Puget Sound region.[11] The soils of the region, less than ten thousand years old, are still characterized as immature.

As the Vashon glacier receded a series of proglacial lakes formed, filling the main trough of Puget Sound and inundating the southern lowlands. Glacial Lake Russell was the first such large recessional lake. From the vicinity of Seattle in the north the lake extended south to the Black Hills, where it drained south into the Chehalis River.[12] Sediments from Lake Russell form the blue-gray clay identified as the Lawton Clay. The second major recessional lake was Glacial Lake Bretz. It also drained to the Chehalis River until the Chimacum Valley, in the northeast Olympic Peninsula, melted, allowing the lake's water to rapidly drain north into the marine waters of the Strait of Juan de Fuca, which was rising as the ice sheet retreated.[12]

The depth of the basins is a result of the Sound being part of the Cascadia subduction zone, where the terranes accreted at the edge of the Juan de Fuca Plate are being subducted under the North American Plate: there has not been a major subduction zone earthquake here since the magnitude nine Cascadia Earthquake; according to Japanese records, it occurred 26 January 1700. Lesser Puget Sound earthquakes with shallow epicenters, caused by the fracturing of stressed oceanic rocks as they are subducted still cause great damage. The Seattle Fault cuts across Puget Sound, crossing just north of Vashon Island and dipping under the city of Seattle.[13] To the south, the existence of a second fault, the Tacoma Fault, has buckled the intervening strata in the Seattle Uplift.

Typical Puget Sound profiles of dense glacial till overlying permeable glacial outwash of gravels above an impermeable bed of silty clay may become unstable after periods of unusually wet weather and slump in landslides.[14]

Transportation

A unique state-run ferry system, the Washington State Ferries, connects the larger islands to the Washington mainland, as well as both sides of the sound, allowing cars and people to move about the greater Puget Sound region.

View southwest from the Space Needle, overlooking (left to right) Elliot Bay, Duwammish Head, Puget Sound, and Restoration Point. Reciprocal view and map can be seen at Seattle Fault.

Flora and fauna

It is estimated that more than 100 million geoducks are packed into Puget Sound's sediments. Also known as "king clam," geoducks are considered to be a delicacy in Asian countries. Orcas are famous throughout the Sound, and are a large tourist attraction. Salmon flow in and out of Puget Sound and are a main food source for many marine animals. Pinnipeds include the harbor seal, the Steller Sea Lion, the California Sea Lion, and the occasional Northern Elephant Seal. Minke, Humpback whale, and Grey Whales also live in the waters.

Prominent islands

See also

References

  1. ^ a b c d Lincoln, John H. "The Puget Sound Model Summary". Pacific Science Center. Retrieved 23 December 2009.
  2. ^ Kruckeberg, Arthur R. (1991). The Natural History of Puget Sound Country. Seattle: University of Washington Press. pp. 427–428. ISBN 0-295-97477-X.
  3. ^ U.S. Geological Survey Geographic Names Information System: Puget Sound
  4. ^ Environmental History and Features of Puget Sound, see also: Map of subareas of Puget Sound, National Oceanic and Atmospheric Administration and National Marine Fisheries Service
  5. ^ a b c Kruckeberg, Arthur R. (1991). The Natural History of Puget Sound Country. Seattle: University of Washington Press. pp. 61–64. ISBN 0-295-97477-X.
  6. ^ Thrush, Coll (2007). Native Seattle: Histories from the Crossing-Over Place. University of Washington Press. p. 220. ISBN 0-295-98700-6.
  7. ^ "Physiographic divisions of the conterminous U. S." U.S. Geological Survey. Retrieved 2007-12-06.
  8. ^ Features of Puget Sound Region: Oceanography And Physical Processes, Chapter 3 of the State of the Nearshore Report, King County Department of Natural Resources, Seattle, Washington, 2001.
  9. ^ Merriam-Webster, Richard (2000). Merriam-Webster's Collegiate Encyclopedia. Merriam-Webster. p. 808. ISBN 9780877790174.
  10. ^ Manning, Richard (2001). Inside Passage: A Journey Beyond Borders. Island Press. p. 113. ISBN 9781559636551.
  11. ^ a b Kruckeberg (1991), pp. 18–23.
  12. ^ a b Baum, Rex L.; Godt, Jonathan W.; Highland, Lynn (2008). Landslides and engineering geology of the Seattle, Washington, area. Volume 20 of Reviews in engineering geology. Geological Society of America. pp. 12–13. ISBN 9780813741208.
  13. ^ "Ancient seismic stresses at work in Puget Sound region" Cyberwest Magazine 9 June 2004
  14. ^ Washington State Department of Ecology:"Puget Sound landslides"

Further reading

  • Jones, M.A. (1999). Geologic framework for the Puget Sound aquifer system, Washington and British Columbia [U.S. Geological Survey Professional Paper 1424]. Reston, VA: U.S. Department of the Interior, U.S. Geological Survey.
  • Prosser, William Farrand (1903). A history of the Puget Sound country : its resources, its commerce and its people : with some reference to discoveries and explorations in North America from the time of Christopher Columbus down to that of George Vancouver in 1792, when the beauty, richness and vast commercial advantages of this region were first made known to the world. Lewis Pub. Co.Available online through the Washington State Library's Classics in Washington History collection

External links

Wikimedia Commons has media related to Puget Sound.

47°36′N 122°27′W / 47.6°N 122.45°W / 47.6; -122.45

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