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Turbidite Hill information


Turbidite Hill (82°1′S 157°45′E / 82.017°S 157.750°E / -82.017; 157.750) is a low nunatak that lies four nautical miles (7 km) east of Laird Plateau on the north side of Olson Neve in Antarctica. It was mapped by the Holyoake, Cobham and Queen Elizabeth Ranges party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1964–65). It was named after sedimentary features, called turbidites, which were reportedly found in sedimentary rocks of the Beacon Supergroup which forms the summit of this hill.[1][2][3]

  1. ^ United States Geological Survey (nd) Turbidite Hill. Geographic Names Information System, U.S. Department of the Interior, U.S. Geological Survey, Reston, Virginia.
  2. ^ Stewart, J. (2011) Antarctic An Encyclopedia McFarland & Company Inc, New York. 1776 pp. ISBN 9780786435906.
  3. ^ Laird, M.G., G.D. Mansergh and J.M.A. Chappell (1971) Geology of the central Nimrod Glacier area, Antarctica. New Zealand Journal of Geology and Geophysics 14(3):427–468.

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Turbidite Hill

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Turbidite Hill (82°1′S 157°45′E / 82.017°S 157.750°E / -82.017; 157.750) is a low nunatak that lies four nautical miles (7 km) east of Laird Plateau...

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Turbidity current

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water column. The sedimentary deposit of a turbidity current is called a turbidite. Seafloor turbidity currents are often the result of sediment-laden river...

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Aravalli Range

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with average width of 40 km carbonate-free phyllite and arenite with turbidite facies and argillaceous rocks. Udaipur Group is a thick accumulation of...

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New Zealand Geological Survey Antarctic Expedition

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Haughmond Hill

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summit overlooks countryside and Shrewsbury itself. Haughmond Hill is made up of ancient turbidite sediments from the late Precambrian era which once cascaded...

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Madeira Abyssal Plain

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composition, the turbidites have been divided into three groups. First, there are a group of organic-rich turbidites. These turbidites represent organic-rich...

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(Welsh: Bryniau Clwyd; also known as the Clwydian Hills; or simply the Clwyds) is a series of hills in the north-east of Wales that runs from Llandegla...

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Sole markings

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and paleocurrent indicators. Sole markings are found most commonly in turbidite deposits, but are also often seen in modern river beds and tidal channels...

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Mynydd Mallaen

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is an outcrop of conglomerate turbidite rock on the western limb of the Cothi Anticline which forms the summit of the hill. Glacial till and boulder clay...

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Mount Thullier

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Nicobar Islands. The mountain is composed of parallel ridges of folded turbidite sandstone. The island's five perennial rivers – the Galathea, Jubilee...

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Geology of Bermuda

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crust around the island is about 120 million years old. Volcaniclastic turbidite deposits 140 kilometers offshore to the southeast indicate that Bermuda...

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Olympic National Park

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The park is known for its unique turbidites. It has very exposed turbidities with white calcite veins. Turbidites are rocks or sediments that travel...

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Crag Hill

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laminated mudstone and siltstone. Beneath this are the Greywacke sandstone turbidites of the Loweswater Formation. The Causey Pike Fault runs across the southern...

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The Bahamas

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such as Great Bahama Canyon with the evidence of turbidity currents and turbidite deposition.: 33–40, 65, 72–84, 86  The stratigraphy of the islands consists...

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Geology of Victoria

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near Swan Hill. Central and western Victoria comprise world-class vein-hosted gold deposits, hosted mostly in the extensive Ordovician turbidites. The southeast...

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Ramsey Island

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Llundain Formation. These tuffs arose as volcanic ash falls, ash flows and turbidite deposits. Smaller areas of dark grey mudstones interbedded with debris...

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Elenydd

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but northwest of this structure is the complex Central Wales Syncline. Turbidite mudstones of the lower Silurian Cwmere Formation occur around Caban-coch...

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Kermadec Trench

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to the north. The Kermadec Trench has a southern continuation in the turbidite-filled Hikurangi Trough, but a series of seamounts on the Australian Plate...

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Sedimentary structures

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dropped out of the current. The most common place to find this is in a turbidite deposit. This can also be inverted, called reversed graded bedding, and...

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Great Valley Sequence

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Individual sandstone beds within these fans and canyons are typically turbidites and related sediment gravity flow deposits, such as the chaotic, often...

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and in the Central Range, uplift has raise the Point-a-Pierre Formation turbidite flysch of the same age. Clastic material and conglomerate marked a shift...

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Dalradian

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and semipelites. The Tayvallich Subgroup contains volcanics within a turbidite basin and there are lavas within the overlying Southern Highland Group...

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Geology of the United States Virgin Islands

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Late Cretaceous, the overlying Tutu Formation took shape with volcanic turbidite and rare pyroxene basalt. Silt or sand-sized material is most common unlike...

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Limestone

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(Globigerina ooze) to silicic mud lacking carbonates. In rare cases, turbidites or other silica-rich sediments bury and preserve benthic (deep ocean)...

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Geology of the Australian Capital Territory

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Camp Hill Sandstone lying on top. There is probably up to 200 metres thickness of this shale. The shale was deposited in the deep sea as turbidites. It...

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Sedimentation

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Katharine & Bursztynsky, Taras A. Erosion & Sediment Control Handbook. McGraw-Hill (1986). ISBN 0-07-023655-0. pp. 8.2, 8.12. Hammer, Mark J. Water and Waste-Water...

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