Coastal morphology and sedimentation, lower Cook Inlet, Alaskawith emphasis on potential oil spill impacts
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Alaska Dept. of Fish and Game, Marine/Coastal Habitat Management , Anchorage, Alaska
Coasts -- Alaska -- Cook Inlet Region, Coasts -- Alaska -- Kachemak Bay Region, Sedimentation and depo
Alaska, Cook Inlet Region., Kachemak Bay Re
|Statement||by Miles O. Hayes, P. Jeffrey Brown & Jacqueline Michel.|
|Series||Environmental studies of Kachemak Bay and lower Cook Inlet ;, v. 2|
|Contributions||Brown, P. Jeffrey., Michel, Jacqueline., Alaska. Marine and Coastal Habitat Management.|
|LC Classifications||QH105.A4 E6 1977 vol. 2, GB458.7 E6 1977 vol. 2|
|The Physical Object|
|Pagination||107 leaves :|
|LC Control Number||79620833|
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Coastal morphology and sedimentation, lower Cook Inlet, Alaska: with emphasis on potential oil spill impacts [Miles O.
Brown, P. Coastal morphology and sedimentation. ; Michel, Jacqueline Author: Hayes, Miles O. Brown, P. Jeffrey. ; Alaska book, Jacqueline; ; Alaska. lower Cook Inlet Coastal morphology and sedimentation, lower Cook Inlet, Alaska: With emphasis on potential oil spill impacts (Environmental studies of Kachemak Bay and lower Cook Inlet) [Miles O Hayes] on *FREE* shipping on qualifying offers.
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Coastal morphology and sedimentation, lower Cook Inlet, Alaska, with emphasis on potential oil spill impacts. [Miles O Hayes; P Jeffrey Brown; Jacqueline Michel; Alaska. Marine and Coastal Habitat Management,]. Buy Coastal morphology and sedimentation, lower Cook Inlet, Alaska: With emphasis on potential oil spill impacts (Environmental studies of Kachemak Bay and lower Cook Inlet) by Miles O Hayes (ISBN:) from Amazon's Book Store.
Author: Miles O Hayes. Buy Coastal morphology and sedimentation, lower Cook Inlet, Alaska: With emphasis on potential oil spill impacts (Technical report - University of South Carolina, Coastal Research Division ; no.
CRD) by Miles O Hayes (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Miles O Hayes.
“A Coast Beyond Compare is an amazing book: a textbook, a reference book and an art book in one. Beautifully illustrated, it honors one of the world’s most spectacular coastlines. The book covers the evolution Alaska coast from the beginning of the universe (really!) to the puts the coast in context of global plate tectonics and right down to centimeter-scale ripples.
This highly active tectonic setting is the dominant influence on the nature of the depositional systems and the sediment composition along the inlet's shoreline.
The km of shoreline of Lower Cook Inlet was subdivided into erosional (45%), neutral (38%), and depositional (17%) by: Cook Inlet (Fisher and Magoon ) and the Sea of Okhotsk (Watson and FujitaEichelberger et al. ) occur within back-arc settings in which extensional tectonics are operative.
The Gulf of Cambay occupies a rift basin that was formed in the early Mesozoic during and after the separation of India from Gondwanaland (Biswas ).
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Shoreline Sedimentation within a Forearc Embayment, Lower Cook Inlet, Alaska. Miles O. Hayes, Jacqueline Michael. ABSTRACT. Lower Cook Inlet is a forearc embayment associated with the northeast extension of the Aleutian volcanic arc.
This highly active tectonic setting is the dominant influence on the nature of the depositional systems and the. Click on the book chapter title to read more. The Castle Mountain fault is a km-long, right-lateral fault that forms the northern boundary of the Cook Inlet basin and Matanuska Valley, Alaska.
Fault gouge and fault rock at six localities contain the clay minerals illite, smectite, chlorite, and interstratified illite/smectite. A regional classification of shoreline segments along the Alaskan Beaufort Sea Coast was developed as the basis for quantifying coastal morphology, lithology, and carbon and mineral sediment fluxes.
We delineated 48 mainland segments totaling 1, km, as well as 1, km of spits and islands. Mainland coasts were grouped into five broad classes: exposed Cited by: Offshore tracts in Alaska's lower Cook Inlet are scheduled to be opened for exploratory petroleum drilling in the near future.
Because of the potential for oil spills resulting from this activity, a field study of the coastal zone was conducted in June A total of km of shoreline was classified into 3 types: erosional (45 percent), neutral (38 percent), and Cited by: Coastal morphology and sedimentation, lower Cook Inlet, Alaska, with emphasis on potential oil spill impacts: Tech.
Rept. CRD, Coastal Research Division P J Brown J Michel. Download full text in PDF Download. Share. ExportCited by: 3. The Study Area - Cook Inlet, Alaska Cook Inlet is a positive, partially-mixed estuary located north of the Gulf of Alaska in the southcentral portion of the state in an area surrounded by mountains and glaciers (Figure 1).
The inlet is some I S j km long in a northeast-southwest direction, and km in width at the mouth. coastline in western lower Cook Inlet, a large tidal estuary with a length of km and a width ranging from about 20 to 90 km.
It is bordered on the west and northwest by the Alaska Range, on the northeast by the Talkeetna Mountains, and on the southeast by the Kenai-Chugach Mountains.
Cook Inlet is an extremely dynamic, high-energy. Co-seismic subsidence occurred over an elongate region including the Kenai Peninsula and most of Cook Inlet. In greater Anchorage, the largest urban area in Alaska, co-seismic subsidence ranged from m (Plafker, ).
Girdwood, the main site reported in this paper, experienced ∼ m regional subsidence in AD and up to Cited by: For more information, contact the Center for Alaskan Coastal Studies, P.O.
BoxHomer, AK or [email protected] 4 Red Algae Alaria Soft Brown Kelp Dark Brown Kelp Dragon Kelp Eelgrass Bull Kelp Shore Modifications Western Lower Cook Inlet Photo Points Western Lower Cook Inlet Environmental Data Kodiak Island Photo Points. Augustine Volcano, a small island volcano located in Cook Inlet, Alaska has produced approximately 11 flank-failure debris-avalanches over the last 2, yrs (BP) that were large enough to reach the coast of the island and enter the sea.
Each debris avalanche conceivably could have triggered a tsunami. Ina tsunami generated by an eruption and flank-failure. Not only have the beaches eroded quickly during the past years, but erosion rates have increased significantly over time. The greatest changes have been observed along the tribal reservation, where USGS scientists and their collaborators reported in a article that erosion averaged nearly 2 ft per year between and (see Warrick and others.
A Unified Sediment Transport Formulation for Coastal Inlet Application; Data Report: Laboratory Testing of Longshore Sand Transport by Waves and Currents; Morphology Change Behind Headland Structures.
Shift-Click here to download the file - ( MB) Laboratory Study of Wind Effect on Runup over Fringing Reefs, Report 1: Data Report. By continuing to browse this site you agree to us using cookies as described in About Cookies.
Remove maintenance message. Open navigation Open search. Skip to main content; Log in / Cited by: 7. Three seismic reflectors are present throughout the lower Cook Inlet basin and can be correlated with onshore geologic features.
The reflections come from unconformities at the base of the Tertiary sequence, at the base of Upper Cretaceous rocks, and near the base of Upper Jurassic strata. A contour map of the deepest horizon shows that Mesozoic rocks are formed into a. REFERENCES recorded in a metre core, Can. Earth Sci., 20,Boothroyd, J.C., Coarse-grained sedimentation on a braided outwash fan, northeast Gulf of.
Circulation in the lower Cook Inlet region has been described and discussed utilizing current observations obtained during October October The major circulation feature was a mean westerly flow which entered the region via Kennedy and Stevenson entrances, paralleled the m isobath through the lower Inlet then exited the system viaFile Size: KB.
Orlando, Robert. Sedimentology and bedform Morphology in Lower Cook Inlet, Alaska. 75 p. Orris, Greta. A quantitative investigation of landslides in a portion of the Santa Clara formation, Santa Clara County, California ().
80 p. Schwartz, David.
Description Coastal morphology and sedimentation, lower Cook Inlet, Alaska PDF
In addition, Cook Inlet exhibits the largest tidal fluctuations in the United States, and as a result, the nearshore regions encounter significant flooding and drying which poses threats to a variety of activities in the coastal regions.
A coupled wind-wave-current system is developed to obtain daily forecasts of waves and circulation patterns. of lower Cook Inlet are: Kenai Peninsula, to 2, Kamishak Bay Shelikof Strait, to 2, and Kodiak Archipelago, to 6, The estimated sea otter population of Alaska istoCook Inlet in Alaska has been identified as a prime site in the U.S.
for potential tidal energy development, because of its enormous tidal power potential that accounts for nearly one-third of the national total. As one important step to facilitate tidal energy development, a tidal hydrodynamic model based on the unstructured-grid, finite-volume community ocean model.
The scope of this project included lower Cook Inlet, Norton Sound and the southern part of the Chukchi Sea in addition to the three shelf areas (Gulf of Alaska, S.
Bering and Beaufort Seas). Baseline collection and analysis of water column samples is .Port of Anchorage is located in lower Knik Arm, a macrotidal subestuary of Cook Inlet, Alaska characterized by large, seasonally variant suspended sediment loads; strong tidal currents; and dynamic eddy structure associated with headland points and shoals.Kelp beds are an example of an abundant and essential nearshore habitat type in coastal Alaska.
Kelps are the foundation organisms of these complex, three-dimensional habitats that support tightly linked food webs (Dayton, ; Fredriksen, ; Mann, ).Cited by:
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