2 edition of Surficial geology of the eastern Gulf of Maine and Bay of Fundy found in the catalog.
Surficial geology of the eastern Gulf of Maine and Bay of Fundy
Gordon B. Fader
by Fisheries and Environment Canada, Fisheries and Marine Service in Ottawa
Written in English
|Statement||by Gordon B. Fader, Lewis H. King and Brian MacLean.|
|Series||Paper - Geological Survey of Canada ; 76-17, Marine sciences paper ; 19|
|Contributions||King, Lewis H., MacLean, Brian., Canadian Hydrographic Service.|
|The Physical Object|
|Pagination||iv, 23 p. :|
|Number of Pages||23|
Maps, Publications and Online Data Search. The Maps and Publications Search allows you to find maps and publications by geographic area or subject.; The Maps and Publications Catalog (PDF 14MB) allows you to browse for maps and publications available from the Maine Geological Survey.; Online Maps. Over geologic quadrangle maps and publications are now available . This was not the case in the Gulf of Maine and Bay of Fundy, where vigourous ice stream drawdown cleared ice from these regions leaving a glacio-isostatically depressed landscape. Before the land rebounded, beaches, and deltas formed that have been radiocarbon dated between 15 (~ CAL) and ka (~15 CAL).
This "White Head Island horst" is bound on its eastern side by the submerged Grand Manan Fault, which lies within the Bay of Fundy and provides a southwestern border for the larger Fundy Basin (Fig. 1). of the Bay of Fundy and into Maine, New Hampshire, and Massachusetts. Cape Cod has glacial deposits of sand and gravel, and sandstone and mudflats are found at the head of the Bay of Fundy (Tyrrell, ) Today much of New Brunswick, Maine, New Hampshire and Massachusetts are still rebounding from the glacial.
This report contains surficial sediment data from previously unpublished data sources or from gray literature. These data have been compiled as part of the National Benthic Habitats and Marine Aggregate Resources and Processes Projects to update the existent maps on surficial sediment distribution available for the Gulf of Maine region. Explore Maine Geology. Choose one of the following topics to explore the world of Maine geology. Each subject area includes virtual geology tours, field localities, frequently asked questions, fact sheets, and links to other online resources.
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Get this from a library. Surficial geology of the eastern Gulf of Maine and Bay of Fundy. [Gordon B Fader; Lewis H King; Brian MacLean, (Marine geologist); Canadian Hydrographic Service.].
Surficial Geologic History of Maine. The ice margin withdrew from the Gulf of Maine to the present position of the Maine coast by 17, to 16, years ago (Borns and others, ).Retreat of a tidewater margin of the Laurentide ice sheet in eastern coastal Maine between ca. and 14C yr B.P.: Geological Society of.
The Gulf of Maine (French: Golfe du Maine) is a large gulf of the Atlantic Ocean on the east coast of North is bounded by Cape Cod at the eastern tip of Massachusetts in the southwest and by Cape Sable Island at the southern tip of Nova Scotia in the northeast.
The gulf includes the entire coastlines of the U.S. states of New Hampshire and Maine, as well as Massachusetts north of River sources: Saint John River, Penobscot River. Substrates. The Gulf of Maine has a variety of substrate, including exposed bedrock, gravel, sand, mud, clay, and silt.
These bottom types are patchily distributed across water depths, resulting in. In book: Voyage of Discovery: Fifty years of marine research at Canada’s Bedford Institute of Oceanography (pp–) Sur cial geology of the eastern. Gulf of Maine and the Bay of Fundy. The Bay of Fundy–northern Gulf of Maine region surrounds the southern part of Nova Scotia, encompassing, from west to east, the Bay of Fundy, Grand Manan Basin, German Bank, Browns Bank, Northeast Channel and northeastern Georges Bank (Fig.
1a, b). During the last glacial maximum (c. 24–20 14C ka BP), the SE margin of the Laurentide Ice Sheet (LIS) occupied the study area, the rest.
Marine Geology, 89 () 69 85 69 Elsevier Science Publishers B.V., Amsterdam -- Printed in The Netherlands MICROTOPOGRAPHY AND SURFICIAL SEDIMENT PATTERNS IN THE CENTRAL GULF OF MAINE: A kHz SURVEY AND INTERPRETATION CHARLES E.
McCLENNEN Department of Geology, Colgate University, Hamilton, NY (U.S.A.) (Received Febru. Surficial geology of the eastern Gulf of Maine and Bay of Fundy.
Canadian Hydrographic Service, Marine Science Pa and Geological. A Geologic History of the Gulf of Maine. Contributed by Abigail Manahan Bigelow Laboratory for Ocean Sciences West Boothbay Harbor, ME The Gulf of Maine, sometimes referred to as a “sea within a sea,” extends 7, miles from Cape Cod to Cape Sable, Nova Scotia.
The Gulf of Bothnia (/ ˈ b ɒ θ n i ə /; Finnish: Pohjanlahti; Swedish: Bottniska viken, also divided as Bothnian Bay + Bothnian Sea) is the northernmost arm of the Baltic is situated between Finland's west coast and Sweden's east coast. In the south of the gulf lie the Åland Islands, between the Sea of Åland and the Archipelago Sea.
Bivalve reefs are important in pelagic–benthic coupling and, in order to assess these linkages quantitatively, it is necessary to obtain accurate maps of reef biomass and production. Presented here is a preliminary attempt to use modern surficial geological techniques, including sidescan sonar and a high resolution seismic reflection system to map the distribution of bivalve reefs in the Bay.
Channel with Minas Basin, (Figure 2). Minas Channel connects with the inner Bay of Fundy to the west. The Bay of Fundy is part of a much larger regional marine system that includes the Gulf of Maine and Georges Bank and is referred to as the FMG for research purposes. The Bay of the Fundy is a linear embayment, km in length that tapers to Presented here is a preliminary attempt to use modern surficial geological techniques, including sidescan sonar and a high resolution seismic reflection system to map the distribution of bivalve reefs in the Bay of Fundy.
Acoustic techniques were groundtruthed with a m 2 video grab. The grab jaws could be hydaulically closed from the. Submarine glacial landforms on the Bay of Fundy-northern Gulf of Maine continental shelf Article (PDF Available) in Geological Society London Memoirs 46(1) December with Reads.
Year Published: Submarine glacial landforms on the Bay of Fundy–northern Gulf of Maine continental shelf. The Bay of Fundy–northern Gulf of Maine region surrounds the southern part of Nova Scotia, encompassing, from west to east, the Bay of Fundy, Grand Manan Basin, German Bank, Browns Bank, Northeast Channel and northeastern Georges Bank (Fig.
1a, b). Distribution and geologic structure of Triassic rocks in the Bay of Fundy and the northeastern part of the Gulf of Maine. U.S. Geological Survey Professional paper B. BB Todd, B.J. and Shaw, J.
Surficial Geologic Map of Maine edited by Woodrow B. Thompson and Harold W. Borns, Jr. 42" x 52" color wall map. View the map. This map is also available in print: Price: $ A 42" x 52" color wall map showing the surficial geology of Maine.
Includes sites of special interest, radiocarbon-dated sites, reference list, correlation chart, inset. Publication_Date: Title: Surficial Geology of the Maine Inner Continental Shelf Publication_Information: Publication_Place: Augusta, ME Publisher: Maine Geological Survey Online_Linkage: Source_Scale_Denominator:Type_of_Source_Media: Source_Time_Period_of_Content: Time_Period_Information: Range_of_Dates/Times: Beginning_Date.
Surficial geology of the inner continental shelf of the northwestern Gulf of Maine: Piscataqua River to Biddeford Pool. Maine Geological Survey Geologic Map, no.———.
Surficial geology of the inner continental shelf of the northwestern Gulf of Maine. Contact. Department of Agriculture, Conservation and Forestry 22 State House Station 18 Elkins Lane Augusta, ME More Locations.
Phone: () Fax: (). The geology of Massachusetts includes numerous units of volcanic, intrusive igneous, metamorphic and sedimentary rocks formed within the last billion years.
The oldest formations are gneiss rocks in the Berkshires, which were metamorphosed from older rocks during the Proterozoic Grenville orogeny as the proto-North American continent Laurentia collided against proto-South America.MAINE’S STATE FOSSIL.
Pertica quadrifaria. Pertica quadrifaria is the scientific name of a primitive plant that lived about million years ago during the Devonian Period. For more information, visit the Maine Geological Survey’s web page on Pertical quadrifaria.From there you can reach most Bay of Fundy locations within a hour drive.
Keep in mind that it’s a very large area and viewing tides will take up a good chunk of time. The Bay of Fundy is on the west side of Nova Scotia, but the north and east side of Nova Scotia are also very nice places to go sailing. Kevin