Encyclopedia
| Puget Sound
Encyclopedia
|
| Tutorials | Encyclopedia | Dictionary | Directory |
|
Puget Sound
Puget Sound
Name and definitionThere 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, then 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]. Another neologism also popularized by environmental and aboriginal groups is Salish Sea, but this does not have wide acceptance nor a single standard meaning from one group to the next. 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] HistorySee also Puget Sound region. 
Evening on Puget Sound by Edward S. Curtis, 1913 After arriving along the Oregon Trail, many settlers wandered north to what is now Washington State and settled the Puget Sound area. The first non-Aboriginal 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. Geology
Low Tide Whidbey Island Puget Sound is a very large salt water estuary, or system of many estuaries, fed by highly seasonal freshwater from the Olympic and Cascade Mountain watersheds.[8] The northern boundary is Admiralty Inlet, between Point Partridge on Whidbey Island and Point Wilson on the Olympic Peninsula. A second entrance is Deception Pass, between West Point on Whidbey Island and Rosario Head on Fidalgo Island.[9] The Sound has been reshaped by the scouring action and till deposition of the Wisconsin Glaciation, which extended in this region as far south as Olympia; the soils of the region, less than ten thousand years old, are still characterized as immature. During glacial maximum a large meltwater lake formed at the icewall's forefront, drained by the Chehalis River; its sediments form the blue-gray clay identified as the Lawton Clay. As icebergs calved off the toe of the glacier, their embedded gravels and boulders were deposited in the chaotic mix of unsorted till geologists call glaciomarine drift. Many beaches about the Sound display glacial erratics, rendered more prominent than those in coastal woodland solely by their exposed position; submerged glacial erratics sometimes provide hazards to navigation. The sheer weight of glacial-age ice depressed the landforms, which experienced isostatic rebound after the ice sheets had retreated; because the rate of rebound was not synchronous with the post-ice age rise in sea levels, the bed of what is Puget Sound, filled alternately with fresh and with sea water. The upper level of the lake-sediment Lawton Clay now lies about 120 feet (37 m) above sea level. 
Snowcapped peaks are a backdrop to many Puget Sound scenes; here Mount Rainier is seen from Gig Harbor. 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 [11]. 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.[12] GeographyA 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. Flora and faunaGeoduck: 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. Prominent islands
U.S. Navy Bases
Puget Sound in music and movies
See also
ReferencesFurther reading
External links
da:Puget Sound de:Puget Sound eo:Pu?eta Fjordo fr:Puget Sound id:Puget Sound ms:Puget Sound nl:Puget Sound ja:???????? pl:Zatoka Puget sv:Puget Sound vo:Puget Sound zh:????? Source: Wikipedia | The above article is available under the GNU FDL. | Edit this article
|
|
top
©2008-2009 TutorGig.com. All Rights Reserved. Privacy Statement
