1 edition of Ground-water flooding in glacial terrain of southern Puget Sound, Washington. found in the catalog.
Ground-water flooding in glacial terrain of southern Puget Sound, Washington.
by U.S. Dept. of the Interior, U.S. Geological Survey in [Reston, Va.?
Written in English
|Other titles||Ground water flooding in glacial terrain of southern Puget Sound, Washington.|
|Series||USGS fact sheet -- 111-00., Fact sheet (Geological Survey (U.S.)) -- FS-00-111.|
|Contributions||Geological Survey (U.S.)|
|The Physical Object|
|Pagination|| p. :|
South Puget Sound is a land of gentle terrain and shallow inlets. Hood Canal, on the other hand, is steep and deep: steep mountains above, deep waters below. It’s a genuine glacier-carved fjord, the only one in the continental United States. The Puget Lowland is subject to seismic shaking from great megathrust subduction earthquakes, most recently in A.D. Figure 1. Image calculated from lidar topography of part of the Seattle fault zone, 15 km west of Seattle. Scene is km across. See Figure 3 for location. High-Resolution Lidar Topography of the Puget Lowland, WashingtonCited by:
Flooding may occur as an overflow of water from water bodies, such as a river, lake, or ocean, in which the water overtops or breaks levees, resulting in some of that water escaping its usual boundaries, or it may occur due to an accumulation of rainwater on saturated ground in an areal flood. Part or all of this report is presented in Portable Document Format (PDF); the latest version of Adobe Reader or similar software is required to view it.
Glacial Lake Carbon was a lake created by the Puget Lobe damming the Carbon River. Around 16, BP when the glacier began retreating, the ice dam holding back the lake became breached causing a major glacial outburst flood. The flood covered present day central and northern Thurston County, Continent: North America. before and after (scroll right for the present) Click on image to download it. This is our biggest pretty image as of 8/29/ It is by meter pixels, .
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Ground-Water Flooding in Glacial Terrain of Southern Puget Sound, Washington Figure 1. Proglacial Lake Puyattup and successive Lake Spillways (modified from Thorson, ).
Ground-water flooding happens in low-lying areas when the water table rises above the land surface. In the complex glacial geologic framework ofCited by: 2. Ground-water flooding in glacial terrain of southern Puget Sound, Washington Fact Sheet By: Myrtle A.
Jones, Joseph L. Jones, and Theresa D. Olsen. Ground-water flooding happens in low-lying areas when the water table rises above the land surf ace. In the complex glacial geologic framework of southern Puget Sound, this phenomenon can occur along former outwash channel depressions after two or more conse cutive years of abo ve-average precipitation.
It has. Get this from a library. Ground-water flooding in glacial terrain of southern Puget Sound, Washington. [Geological Survey (U.S.);]. Buy Ground-water flooding in glacial terrain of southern Puget Sound, Washington (SuDoc I ) by U.S.
Geological Survey (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible dr-peshev.com: U.S. Geological Survey. Glacial Terrain What Causes Ground-Water Flooding.
the Puget Sound area starting about 18, years ago: It left behind distinctive features such as ice contact depressions and outwash channels that are visible on the shaded relief map of Southern Puget Sound, Washington shown above.
In. Ground-Water Flooding in Glacial Terrain of Southern Puget Sound, Washington, USGS Fact SheetSeptember Describe the process that formed the glacial outwash channels in Pierce County, such as the South Tacoma Channel. Describe the. Many narrow inlets of Puget Sound form most of the northern boundary.
The county is adjoined on the northwest by Mason County, on the west by Grays Harbor County, and on the south by Lewis County. Olympia, the county seat and State capital, is in the north-central part of Thurston County.
Glacial Lakes of the Puget Lobe Over the last several million years, glaciers have repeatedly inundated northern Washington. The last glacial climatic interval was called the Fraser glaciation, which sculpted much of the topography we see today in the Puget Lowland and northern Washington.
Southern Cascades; Olympic Mountains; Willapa Hills; Columbia Basin; Blue Mountains; Puget Lowland; Portland Basin; Puget Sound, Coastal Geology; Geology Glossary; Glacial Geology; Rockhounding; Geologic Hazards.
Earthquakes and Faults. School Seismic Safety; Landslides. Climate Resilience for Washington ; DNR's Strategic Plan ; Boards and. 2 GEOLOGY AND GROUND-WATER RESOURCES, THURSTON CO., WASH. Location and Extent of the Area Thurston County is in western Washington at the southern end of Puget Sound (pl.
The total area of the county is approximately square miles, which lies within Tps. 15to20 N. and Rs. to3 E. of the Willamette. Ground-water flooding in glacial terrain Water-Resources Investigations Report By: Myrtle Jones, Joseph Jones, and Theresa Olsen.
Western Washington is hilly and even mountainous in places with lots of rivers and lakes. This includes the three lakes that dictate the geography of the greater Seattle metropolitan area: Lakes Union, Washington and Sammamish.
This same glacial activity also created the many islands that dot the Strait of Juan de Fuca and Puget Sound. This Puget Sound data was used as an example dataset in this paper: "Visualization of Large Terrains Made Easy" Peter Lindstrom and Valerio Pascucci IEEE Visualization '01 Conference Proceedings October Full Acknowledgements: Data is obtained from The United States Geological Survey (USGS), made available by The University of Washington.
A flood is an overflow of water that submerges land that is usually dry. In the sense of "flowing water", the word may also be applied to the inflow of the dr-peshev.com are an area of study of the discipline hydrology and are of significant concern in agriculture, civil engineering and public health.
Flooding may occur as an overflow of water from water bodies, such as a river, lake, or ocean. Ground-water Flooding in Glacial Terrain of Southern Puget Sound, USGS Fact Sheet Shallow Ground-water flooding (Acrobat (PDF) kB Jan28 11) 3) KMZ files for exercise KMZ of Tacoma area topography Shaded relief Tacoma (KMZ File kB Apr14 11).
The Puget Sound is a large body of water that is located on the western side of Washington state in the Pacific Northwest. It lies in the middle of the Olympic and Cascade Mountains. This area was affected by glaciation in the Pleistocene Age around 20, to 25, years B.P. (before present).
ADU - Urban Hydrologic and Geologic Hazards in Puget Sound, Washington. Problem - Current hazards programs of the USGS focus on understanding and monitoring the physical processes that result in individual natural hazards and on producing assessments of these geologic and hydrologic dr-peshev.com the Puget Sound basin, hazards that are especially common and also have a high propensity for.
Many glacial erratic boulders (often simply called glacial erratics) can be found in the Puget Sound region as far south as the Yelm area where the Puget Lobe of the glacier reached its maximum extent. The Pleistocene ice age glaciation of Puget Sound created many.
Sep 24, · About 16, years ago, the Vashon glacier begins to melt and recede from lands that will come to be known as the Puget Sound region and the Columbia Basin region.
By 15, years ago, the glacier has retreated to the border of present-day Canada. understanding earthquake hazards in southern California.
I  Ground -water flooding in glacial terrain of southern Puget Sound, Washington I  The National Flood -Frequency Program --methods for estimating flood magnitude and frequency in rural areas in Arizona. I A flood is an overflow of water that submerges land that is usually dry. In the sense of "flowing water", the word may also be applied to the inflow of the tide.
Floods are an area of study of the discipline hydrology and are of significant concern in agriculture, civil engineering and public hea.Glaciers filled and leveled the region, gouging out channels and trenches that later would become such terrain features as Puget Sound, Lake Washington and Hood Canal.
Ice-borne "erratic" rocks from British Columbia have been found in the low country east of Puget Sound and on the islands within the sound and Admiralty Inlet.