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Skaneateles Formation

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Isochore map of the Stafford Member of the <b>Skaneateles</b> <b>Formation</b>. The dashe...
Published: 01 January 2011
Figure 17 Isochore map of the Stafford Member of the Skaneateles Formation. The dashed isochore represents the mapped zero line of the Stafford Member; elsewhere, contouring is limited by a lack of data. Isochore lines were not traced into the valley and ridge because of sparse data
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Isochore map of the Levanna Member of the <b>Skaneateles</b> <b>Formation</b>. The dashed...
Published: 01 January 2011
Figure 18 Isochore map of the Levanna Member of the Skaneateles Formation. The dashed isochore represents the mapped zero line of the Levanna Member; elsewhere, contouring is limited by a lack of data. Isochore lines were not traced into the valley and ridge because of sparse data and structural
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(A) <b>Skaneateles</b> <b>Formation</b> at Moonshine Falls east of Aurora, New York. Look...
Published: 01 July 2009
Figure 11 (A) Skaneateles Formation at Moonshine Falls east of Aurora, New York. Looking south-southeast parallel to J 2 . (A-1, A-2) Neotectonic or exhumation joints parallel J 2 . (B) Union Springs Member of the Marcellus Formation at Union Springs, New York, looking parallel to J 1 joints
Journal Article
Published: 01 January 1968
Journal of Paleontology (1968) 42 (1): 84–87.
...Thomas X. Grasso Abstract A coral bed in the Skaneateles Formation of central New York, here designated the Case Hill Coral Bed, attains a thickness of 1 1/2 to 2 feet. Although it is apparently restricted to the Tully Valley region its exact areal extent is not known. The fauna of the Case Hill...
Journal Article
Journal: GSA Bulletin
Published: 01 July 1984
GSA Bulletin (1984) 95 (7): 814–828.
... of the Onondaga is equivalent to the overlying Delaware Limestone. The Amherstburg and Lucas Formations of the Detroit River Group of Michigan and Ontario can be traced southward across Lake Erie into the lower and middle parts of the Upper Columbus of Ohio. The Amherstburg correlates with the Edgecliff, Clarence...
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP278.5
EISBN: 9781862395268
... at or near the base of the Givetian Stage. From this level, a new, as yet unnamed, species of Parodiceras was also collected. The overlying Skaneateles Formation (Sequence III) contains a number of important goniatites that aid in correlation of units across the basin. The lowest record of goniatites...
FIGURES | View All (9)
Journal Article
Published: 01 May 2018
Journal of Paleontology (2018) 92 (3): 388–397.
... compare variants from three stratigraphic levels (Skaneateles, Ludlowville, and Moscow formations) and from different habitats characterized by lithofacies. The phenotypic variation observed in our data does not amount to an overall directional shift in morphology, i.e., they constitute reversible changes...
FIGURES | View All (6)
Journal Article
Journal: GSA Bulletin
Published: 01 June 1942
GSA Bulletin (1942) 53 (6): 873–888.
...G. ARTHUR COOPER; ALDRED SCOTT WARTHIN Abstract Because of many easily recognized and restricted species, the fauna of the thin Centerfield formation of New York has considerable stratigraphic importance. The fauna is readily traced across New York from Chenango Valley to Erie County and appears...
Journal Article
Journal: GSA Bulletin
Published: 28 February 1935
GSA Bulletin (1935) 46 (2): 195–224.
... in central Pennsylvania: 1 “The authors have followed the Hamilton group from northern New Jersey to central Pennsylvania. Its four formations—Moscow, Ludlowville, Skaneateles, and Marcellus—can be recognized throughout except in New Jersey, where only the lower part of the group is identified, and in Perry...
Journal Article
Journal: GSA Bulletin
Published: 31 August 1933
GSA Bulletin (1933) 44 (4): 757–782.
...BRADFORD WILLARD; ARTHUR B. CLEAVES Abstract Introduction The Hamilton group in Pennsylvania, as in New York, is divisible into four formations: the Moscow, the Ludlowville, the Skaneateles, and the Marcellus. These are partially subdivisible. In studying the group, Cooper’s published data...
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Contact of the Oatka Creek Member, Marcellus <b>Formation</b>, and the overlying S...
Published: 01 January 2011
Figure 14 Contact of the Oatka Creek Member, Marcellus Formation, and the overlying Stafford Member of the Skaneateles Formation exposed on Oatka Creek, village of LeRoy, New York. TOC of the Oatka Creek Member immediately beneath the contact is 4%. Note heavily jointed nature of the organic-rich
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Sequence-stratigraphic type section of the Marcellus <b>Formation</b> that encompa...
Published: 01 January 2011
Figure 20 Sequence-stratigraphic type section of the Marcellus Formation that encompasses the upper part of the underlying Onondaga Formation and the lower interval of the Skaneateles Formation. TST = transgressive systems tract; RST = regressive systems tract; MFS = maximum flooding surface; MRS
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Wireline log signature of a very thin Union Springs Member as exhibited in ...
Published: 01 January 2011
Figure 6 Wireline log signature of a very thin Union Springs Member as exhibited in the Stowell–Kolb well, Chautauqua County, New York; M = Levanna Member of the Skaneateles Formation; S = Stafford Member of the Skaneateles Formation.
Journal Article
Journal: AAPG Bulletin
Published: 01 January 2011
AAPG Bulletin (2011) 95 (1): 61–103.
...Figure 17 Isochore map of the Stafford Member of the Skaneateles Formation. The dashed isochore represents the mapped zero line of the Stafford Member; elsewhere, contouring is limited by a lack of data. Isochore lines were not traced into the valley and ridge because of sparse data...
FIGURES | View All (34)
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Figure  10. Analyses of horizons within <b>formations</b> of the Hamilton Group us...
Published: 01 November 2009
for this subset owing to the limited number of categories exhibited by these two higher taxa. The Marcellus and Skaneateles Formations are grouped as the Lower Hamilton Group. MDS plots depict relative similarity among horizons, plotted on dimensions 1 (horizontal) and 2 (vertical), and give percentage
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Figure  8. Analyses of samples and horizons within <b>formations</b> of the Hamilt...
Published: 01 November 2009
Figure 8. Analyses of samples and horizons within formations of the Hamilton Group using all taxa; the Marcellus and Skaneateles Formations are grouped as the Lower Hamilton Group. MDS plots depict relative similarity among horizons, plotted on dimensions 1 (horizontal) and 2 (vertical), and give
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Wireline logs illustrating the nature of the top of the Oatka Creek Member–...
Published: 01 January 2011
Figure 16 Wireline logs illustrating the nature of the top of the Oatka Creek Member–Skaneateles Formation contact in the presence (A) and absence (B) of the Stafford Member. Panel (C) illustrates the approach taken in this study to define the contact in more proximal regions of the basin.
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Canonical variate analysis based on shape variations, grouped by facies ( 1...
Published: 01 May 2018
Figure 6 Canonical variate analysis based on shape variations, grouped by facies ( 1 ) and stratigraphic position ( 2 ), all showing 90% confidence ellipses of population mean. fs = fine silt; GIV-1 = Skaneateles Formation; GIV-2 = Ludlowville Formation; GIV-3 = Moscow Formation; s = silt; m
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Maps showing cross-structural discontinuities and (A) the location of the O...
Published: 01 January 2011
Formation; (C) the region of the basin over which the Oatka Creek Member of the Marcellus Formation thins; (D) the distribution of the Stafford Member of the Skaneateles Formation; (E) the distribution of the Levanna Member of the Skaneateles Formation illustrating 0 ft, 5 ft (1.5 m), and 20 ft (6.1 m
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Organic carbon (TOC—total organic carbon), Mo concentration, and degrees of...
in > Geology
Published: 01 June 2009
Figure 1. Organic carbon (TOC—total organic carbon), Mo concentration, and degrees of pyritization (DOP) values suggest that Oatka Creek Formation is more reducing than Geneseo Formation. A: Oatka Creek Formation. U.S.—Union Springs Formation; Skaneat.—Skaneateles Formation. B: Geneseo Formation