4 edition of Coastal morphology and sedimentation, lower Cook Inlet, Alaska found in the catalog.
1977 by Alaska Dept. of Fish and Game, Marine/Coastal Habitat Management in Anchorage, Alaska .
Written in English
Bibliography: leaves 90-95.
|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 :|
|Number of Pages||107|
|LC Control Number||79620833|
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY COASTAL MORPHOLOGY, COASTAL EROSION, AND BARRIER ISLANDS OF THE BEAUFORT SEA, ALASKA By D. M. Hopkins and R. W. Hartz Open File Report This report is preliminary and has not been edited or reviewed for conformity with Geological, Survey standardsCited by: We explored downtown Anchorage and walked the Tony Knowles Coastal Trail, a beautiful mile path that winds along the Knik Arm and the Cook Inlet. The next morning, we boarded our assigned bus, one of several taking excited travelers on a three-hour drive to the Mt. McKinley Princess Wilderness Lodge. A baseline environmental characterization of the embayments and fjords on the Kenai Peninsula, Alaska was conducted using a sediment quality approach based on sediment chemistry, and benthic invertebrate community structure. Sediment toxicity and resident fish body burdens were also assessed at one bay near an abandoned mine site. The study area was subdivided into . PSCharacterization of a Low Gas Pressure Reservoir: Beluga Formation, South Ninilchik Gas Field, Cook Inlet, Alaska* Ela Manuel1, Segun Jebutu1, Weidong Li1, Rolando del Cairo1, Jim Woods1, and David Gorney2. Search and Discovery Article # ()** Posted Aug *Adapted from poster presentation at AAPG Annual Convention and Exhibition, Long .
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Coastal morphology and sedimentation, lower Cook Inlet, Alaska: with emphasis on potential oil spill impacts [Miles O.
Brown, P. Jeffrey. ; Michel, Jacqueline Coastal morphology and sedimentation Hayes, Miles O. Brown, P. Jeffrey. ; Michel, Jacqueline; ; Alaska. Lower Cook Inlet 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.
Get this from a library. 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 lower Cook Inlet (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 ).
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. 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: Alaska Coastal Habitat Web Site Restoration Project Final Report Susan M.
Saupe 1 John Harper 2 1 Cook Inlet Regional Citizens Advisory Council Highland Avenue Kenai, Alaska and 2 Coastal and Ocean Resources, Inc. W. Saanich Rd. Environmental assessment of the Alaskan Continental Shelf. Volume XVI. Hazards. Annual report, 1 April March The waters of Kachemak Bay and lower Cook Inlet are rich with plankton, kelp, and seagrass, which form the base of the food web for the fish, shellfish, marine mammals and seabirds living in this region.
Cook Inlet to understand how changing environmental conditions affect species injured by the Exxon Valdez oil spill and coastal ecosystem.
THE POTENTIAL BENEFITS OF EFFLUENT LIMITATION GUIDELINES FOR COASTAL OIL AND GAS FACILITIES IN COOK INLET, ALASKA Final Report Prepared for: Office of Water Office of Science and Technology Engineering and Analysis Division U.S. Environmental Protection Agency M Street, SW Washington, DC February 6, Cook Inlet in particular is host to the one of the largest tidal ranges in North America as well as a large percentage of the industry and population of Alaska.
There are around 10 areas within Cook Inlet that have a combined technical tidal potential of a few hundred megawatts (MW). This would be around half the average load for the entire. Water circulation in lower Cook Inlet is dominated by the Alaska Coastal Current (ACC) that flows northward along the shores of the Kenai Peninsula until it turns westward and is mixed by the combined influences of freshwater input from upper Cook Inlet, wind, topography, tidal surges, and the coriolis effect (Field and WalkerMMS ).
Seldovia, Alaska Seldovia’s harbor at high tide. Seldovia’s slough at low tide. Storm surges at Outside Beach. Looking west across Seldovia and the bay into lower Cook Inlet.
Major sources for this section include: Susan Woodward Springer’s book, Seldovia, Alaska: An Historical Portrait of Life in Zaliv Seldevoe-Herring. Mudflats or mud flats, also known as tidal flats, are coastal wetlands that form in intertidal areas where sediments have been deposited by tides or rivers.
A recent global analysis suggested they are as extensive globally as mangroves. They are found in sheltered areas such as bays, bayous, lagoons, and ts may be viewed geologically as exposed layers of bay mud. ABSTRACT Short term variability in delta form and process can be partly explained by the relative strength of hydraulic parameters such as river discharge, discharge variability, wave energy flux and tidal range.
However, the calibre or grain size is also important. The amount, mode of transport and grain size of the sediment load delivered to a delta front have a considerable .MP Worden, A.K., Schaefer, J.R., and Mulliken, K.M.,Tephra occurrence in Alaska: a map-based compilation of stratigraphic tephra data: Alaska Division of.