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Whitehall Formation

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Journal Article
Published: 01 March 1981
Journal of Sedimentary Research (1981) 51 (1): 69–72.
...D. M. Rubin; G. M. Friedman Abstract A chert bed in the Whitehall Formation (Cambrian and Ordovician) of eastern New York State is strikingly similar in petrography and inferred origin to Australian and South African silcretes. The chert in the Whitehall, like its Australian and South African...
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Table  1 —Uppermost Cambrian faunas from the <b>Whitehall</b> <b>Formation</b>. Number in...
Published: 01 January 2003
Table 1 —Uppermost Cambrian faunas from the Whitehall Formation. Number in parentheses below sample number is mass (in kg) of acid-disaggregated sample. “P” is present; “A,” abundant
Journal Article
Published: 01 January 2003
Journal of Paleontology (2003) 77 (1): 78–98.
...Table 1 —Uppermost Cambrian faunas from the Whitehall Formation. Number in parentheses below sample number is mass (in kg) of acid-disaggregated sample. “P” is present; “A,” abundant ...
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Figure 2. (A) Stratigraphic sections and lithologic criteria for distinguis...
Published: 01 April 2002
.) and member (m.) names ( Fisher, 1985 ). The Whitehall formation is the characteristic unit consisting of the Whitehall facies and includes the Warner Hill limestone, the cliff-forming limestone in the greater Whitehall region. The Ticonderoga sandstone, Ward siltstone, Whitehall dolostone (within
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—Photomicrograph (crossed nicols) of dusty dolomite euhedra syntaxially ove...
Published: 01 November 1975
Fig. 4 —Photomicrograph (crossed nicols) of dusty dolomite euhedra syntaxially overgrown by clearer dolomite of lithofacies 1 (Great Meadows Formation, Whitehall, New York).
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—Mottled cryptalgalaminite of lithofacies 9; darker areas contain abundant ...
Published: 01 November 1975
Fig. 9 —Mottled cryptalgalaminite of lithofacies 9; darker areas contain abundant detrital quartz and feldspar silt-size particles, lighter areas are dolomite (Fort Ann Formation, Whitehall, New York).
Journal Article
Journal: GSA Bulletin
Published: 01 April 2002
GSA Bulletin (2002) 114 (4): 476–489.
....) and member (m.) names ( Fisher, 1985 ). The Whitehall formation is the characteristic unit consisting of the Whitehall facies and includes the Warner Hill limestone, the cliff-forming limestone in the greater Whitehall region. The Ticonderoga sandstone, Ward siltstone, Whitehall dolostone (within...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 1937
GSA Bulletin (1937) 48 (11): 1573–1588.
...JOHN RODGERS Abstract INTRODUCTION This paper gives the results of a detailed survey of the Paleozoic geology of the Whitehall quadrangle, New York-Vermont, west of the Taconic thrust. Reconnaissance work has been carried northward from this area through a large part of the adjoining Ticonderoga...
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Index map of subject area. Major optically stimulated luminescence (OSL)–da...
Published: 01 July 2013
at shallow depths (solid dots): S—Sorrento; W—Frost-Whitehall, S. Livingston Parish; M—Mandeville; Sl—Smith Borrow Pit, N. Slidell; PB—Port Bienville, Mississippi; local Gulfport barrier sector underlain by Biloxi Formation. F-1—Scotlandville–Denham Springs faults; F-2—Baton Rouge fault belt. General geology
Journal Article
Journal: Economic Geology
Published: 01 December 2018
Economic Geology (2018) 113 (8): 1679–1704.
... sequence of immature sandstone and conglomerate, and an upper sequence of sandstone and laminated carbonaceous siltstone, intruded by several generations of felsic plutons and dikes. Whole-rock geochemical analysis indicates their formation in oceanic island-arc environment, and mantle-like characteristics...
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Journal Article
Published: 19 November 2010
Geological Magazine (2011) 148 (4): 529–557.
...’ and given a formation-level status by Fisher and Hanson ( 1951 ) (locality Rit in Fig. 2 ). The terminal Cambrian Little Falls Formation is an ~ 100 m thick, carbonate-dominated interval in the gently E-dipping sections near Whitehall village (see maps in Taylor...
Journal Article
Journal: GSA Bulletin
Published: 01 May 2012
GSA Bulletin (2012) 124 (5-6): 857–869.
... resulted from decompression accompanied by fluid influx. However, the structures that accommodated this proposed exhumation were previously unrecognized. In this study, we present new structural and geochronologic results from the eastern Adirondack Highlands between Fort Ann and Whitehall, New York ( Fig...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1975
AAPG Bulletin (1975) 59 (11): 2123–2141.
...Fig. 4 —Photomicrograph (crossed nicols) of dusty dolomite euhedra syntaxially overgrown by clearer dolomite of lithofacies 1 (Great Meadows Formation, Whitehall, New York). ...
FIGURES | View All (13)
Journal Article
Published: 01 September 2007
Journal of Paleontology (2007) 81 (5): 841–857.
...BJÖRN KRÖGER; ED LANDING Abstract The Tribes Hill Formation (upper Skullrockian) of New York records the earliest Ordovician diversification of cephalopods, in particular ellesmerocerids, on the east Laurentian, shallow carbonate platform. Revision of this cephalopod fauna on the basis...
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Journal Article
Published: 01 March 1967
Bulletin of Canadian Petroleum Geology (1967) 15 (1): 65–81.
... Lake (8 .4 mmcf/d), and Halfway (0 .5 mmcf/d) Formations (Fig . 2) . A three-mile step out, Canadian Superior Whitehall Inga 10-25-88-24W6, discovered the oil column when it encountered th e Charlie Lake sandstone 33 ft . lower than the gas discovery and tested 4 2 A.P .I . oil from a 12-ft . zone...
Journal Article
Published: 01 September 2002
Bulletin of Canadian Petroleum Geology (2002) 50 (3): 419–440.
... and associated with an abrupt lithological change. The upper formation of the Potsdam Group (Cairnside Formation) is locally missing, possibly due to erosion, and void-filling, spherulitic, chalcedonic cement is developed less than a metre beneath the unconformity. The void-filling, silica cement is interpreted...
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Journal Article
Published: 01 March 1972
Bulletin of Canadian Petroleum Geology (1972) 20 (1): 89–103.
...W. I. White ABSTRACT An accumulation of residual materials occurs at the Palaeozoic erosion surface in west-central Saskatchewan, mainly where Mississippian Madison Group limestones subcrop beneath the Cretaceous Blairmore Formation. This accumulation, known as the Residual Zone, is discontinuous...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1994
AAPG Bulletin (1994) 78 (9): 1360–1371.
... of minerals normally associated with lacustrine deposits, and (4) comparison with surface paleosol exposures. 1 Manuscript received May 20, 1993; revised manuscript received April 29, 1994; final acceptance May 9, 1994. 2 Whitehall Geogroup, Inc., 107 Whitetail Road, Whitehall, Montana 59759...
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Journal Article
Published: 01 February 2000
Mineralogical Magazine (2000) 64 (1): 31–42.
... rocks that host the Golden Sunlight deposit can be divided into two units; the older LaHood Formation, consisting of arkoses, sandstones, conglomerates and carbonaceous black shales and the informally named Bull Mountain Group, which is composed of siltstones, shales, synsedimentary sulphide (primarily...
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Journal Article
Published: 01 February 1979
Quarterly Journal of Engineering Geology and Hydrogeology (1979) 12 (1): 9–29.
... time, and offer less scope for study. In the present paper, the author is concerned largely with the better known and more complete Lower Floodplain Terrace of the Thames. A detailed discussion of the mode of formation of these features would be inappropriate here. The deep hollows are not confined...