3 edition of James Ross Island volcanic group of north-east Graham Land found in the catalog.
James Ross Island volcanic group of north-east Graham Land
P. H. H. Nelson
|Statement||by P.H.H. Nelson.|
|Series||Scientific reports / British Antarctic Survey -- no.54., Scientific reports (British Antarctic Survey) -- no. 54.|
|The Physical Object|
|Pagination||, 64 p.,  p. of plates,  leaves of plates (2 fold) :|
|Number of Pages||64|
|LC Control Number||76011983|
The James Ross Island Volcanic Group of north-east Graham Land. The James Ross Island Volcanic Group of north-east Graham Land P. H. H. Nelson The stratigraphy of part of north-east Graham Land and the James RossI J. S. Bibby , 2 books Brian J. Taylor, 2 books N. Aitkenhead, 1 book M. E. Ayling, 1 book H. J. G. Dartnall, 1 book D. M. Moore, 1 book D. G. Singleton, 1 book I. Mackenzie Lamb.
VOLCANIC AND EROSIVE EVENTS ON AN UPPER VISÉAN CARBONATE PLATFORM, The James Ross Island Volcanic Group of north-east Graham Land. Br. Antarc. Surv. Sci. Rept. Thorarinsson, S. Surtsey – the new island in the North Atlantic. Almenna bokafelagid, Reykjavik. Waters, A. C. Determining the direction of flow in basalts. Am. by: Reference: Nelson, P.N.H..() The James Ross Island volcanic group of north-east Graham Land. Cambridge, British Antarctic Survey, 62pp. Cambridge, British Antarctic Survey, 62pp. (British Antarctic Survey Scientific Reports, 54).
Nelson, P.H.H. The James Ross Island Volcanic Group of North-East Graham Land. British Antarctic Survey Scientific Rep 62 pp. Six million years of glacial history recorded in volcanic lithofacies of the James Ross Island Volcanic Group, Antarctic Peninsula. Palaeogeography, Palaeoclimatology, Palaeoecology , https Cited by: 1. Hobbs Glacier is a glacier situated in a steep, rock-walled cirque at the northwest side of Hamilton Point, and flowing southeast into the southern part of Markham Bay on the east coast of James Ross Island, was first seen and surveyed by the Swedish Antarctic Expedition, –04, under Otto Nordenskiöld, who named it for Professor William H. Hobbs, an American geologist and Coordinates: 64°18′S 57°26′W / °S °W.
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The stratigraphy of part of north-east Graham Land and the James Ross Island Group, (British Antartic Survey. Scientific reports) [J. S Bibby] on *FREE* shipping on qualifying offers. - Buy James Ross Island Volcanic Group of North-east Graham Land (Science Reports) book online at best prices in india on Read James Ross Island Volcanic Group of North-east Graham Land (Science Reports) book reviews & author details and more at Free delivery on qualified : P.H.H.
Nelson. Get this from a library. The James Ross Island volcanic group of north-east Graham Land. [P H H Nelson]. James Ross Island is a massive, dominantly Miocene to Pliocene, shield volcano along the Larsen Rift near the northern tip of the Antarctic Peninsula with more youthful flank tuff cones and other pyroclastic centers.
The glacier-covered Mount Haddington shield volcano forms the m. Scientific Reports, Volumes British The James Ross Island Volcanic Group of North-east Graham Land East Bay diorite dykes entrance point epidote euhedral expedition Faustini Fjord following the SGS gabbro geology Glacier gneisses Graham Land granite granodiorite green groundmass Grytviken HMS Protector hornblende HYDROGRAPHIC.
The Stratigraphy of Part of North−East Graham Land and the James Ross Island Group. British Antarctic Survey Scientific Report 37 pp. BLIKRA L.H. and NEMEC W. Postglacial colluvium in western Norway: depositional pro− cesses, facies and palaeclimatic record.
Sedimentology – CHOUGH S.K. and HWANG I.G. The Duksung. Freshwater lakes of Ulu Peninsula, James Ross Island, north-east Antarctic Peninsula: origin, geomorphology and physical and chemical limnology. Vol Issue 3; The James Ross Island Volcanic Group of north-east Graham Land.
British Antarctic Survey Scientific Reports, 54, 62 Cited by: James Ross Island is located on the northern Antarctic Peninsula. It lies east of the Trinity Peninsula mountains on the Antarctic Peninsula, and these mountains shield the island from precipitation. This is one of the reasons why the island has large ice-free areas.
James Ross Island is a large island off the southeast side and near the northeastern extremity of the Antarctic Peninsula, from which it is separated by Prince Gustav to 1, metres (5, ft), it is irregularly shaped and extends 64 km (40 miles) in a north–south direction.
It was charted in October by the Swedish Antarctic Expedition under Otto Nordenskiöld, who named Highest point: Mount Haddington. The James Ross Island Volcanic Group (JRIVG) is a large (c.
km 2), long-lived (> 6 myr) basaltic volcanic field situated in northern Antarctic Peninsula and dominated by the Mount Haddington stratovolcano (Fig. 1, Fig. It is in a pivotal position (northerly latitude, low elevation) to record the dynamics of the adjacent Antarctic Cited by: A revised stratigraphy of Cenozoic volcanic outcrops in the Brandy Bay area on James Ross Island is obtained by combining palaeomagnetic and stratigraphical anlysis with 40Ar/39Ar dating.
Vol 53 The Stratigraphy of Part of North-East Graham Land and the James Ross Island Group. 37p., fold-out color map, fold-out chart, 5p. b/w Plates. J.S. Bibby, Vol 54 The James Ross Island Volcanic Group of North-East Graham Land. 62p., 3 fold-out maps – 2 in color, fold-out chart, 11p.
b/w Plates, References. Journal reviewers are thanked for their constructive critical reviews. Gill Clarke is thanked for typing numerous drafts of the manuscript. 81 References Bibby, J.S., The stratigraphy of part of North-East Graham Land and the James Ross Island group.
Sci. Cited by: Graham Land, a jagged, glaciated part of Antarctica. An Antarctic cruise may explore the upper tip of the Antarctic Peninsula where one finds Graham Land, a jagged, glaciated part of Antarctica with a landscape dominated by volcanoes. Despite the volcanoes being over million years old they are far from extinct with volcanic activity occurring today.
James Ross Island. The James Ross Island Volcanic Group is a stratigraphic unit of Cenozoic age distributed on James Ross Island and Vega Island of the James Ross Island group, the Tabarin and Trinity peninsulas of Graham Land and surrounding islands in the Prince Gustav and Antarctic sounds.
The volcanic group consists predominantly of alkali basalts with minor hawaiites, benmoreites and mugearites. (a) Steep-sided, mainly volcanic, valley walls of southern and eastern James Ross Island. (b) Glacially-eroded landscape, including flat-top mesas, of northern and western James Ross Island.
References Bibby, J. The stratigraphy of part of north-east Graham Land and the James Ross Island group.
British Antarctic Survey Scientific Repo 37 pp. Crame, J. Upper Cretaceous inoceramids (Bivalvia) from the James Ross Island group and their stratigraphical significance.
British Antarctic Survey Bulle Cited by: SedimentaO' Geology, 71 () Elsevier Science Publishers B.V., Amsterdam Field relationships and stable isotope geochemistry of concretions from James Ross Island, Antarctica Duncan Pirrie a.
and James D. Marshall b British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge CB3 0ET, UK h Department of Earth Sciences, Cited by: The climate of James Ross Island is relatively cold and dry, with a mean annual temperature about -5 (Reynolds, ).
Tumbledown Cliffs, on the western side of James Ross Island, is a ca. 10 km2 large ice-free area, which X/95/$ Elsevier Science by:. The James Ross Island Volcanic Group of north−east Graham Land.
British Antarctic Survey, Scientific Reports 1– Marine terraces of Seymour Island, Antarctic Peninsula.PDF | OnJakub Hrubý and others published Compositional characteristics of olivine in back-arc volcanites from James Ross Island | Find, read and cite all the research you need on.Part 4: Antarctica, Asia and Europe (excluding the former USSR), Australasia and Oceanic Islands.
Geological Society, pages. ; Nelson, P.H.H. () The James Ross Island volcanic group of north-east Graham Land. British Antarctic Survey, Cambridge, (British Antarctic Survey Scientific Reports, 54), 62 pages.