Warley Hill Formation

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Journal Article
Published: 01 November 2000
Journal of Sedimentary Research (2000) 70 (6): 1290–1301.
... be recognized clearly in both downdip and updip areas of the passive margin. Three other sequence boundaries, which occur at the base and top of the Warley Hill Formation and within the Tinker Formation, are interpreted as formed during relative sea-level fall associated with third-order global cycles...
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Journal Article
Published: 22 May 2014
Proceedings of the Yorkshire Geological Society (2014) 60 (1): 29–51.
...C. N. Waters; D. Millward; C. W. Thomas Summary In the Northumberland–Solway Basin and Alston Block of northern England, some aspects of the stratigraphical and sedimentological relationships between the Millstone Grit Group, the Stainmore Formation (Namurian part of the Yoredale Group...
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Core photographs. Length of bar scale is 4 cm.  A)  Very well sorted, mediu...
Published: 01 November 2000
nearshore interval; upper part of Congaree Formation; well MSB2B, 45.9 m. C) Interlaminated clay and silt of transition zone from distal to proximal shelf; Warley Hill Formation; well MSB1C, 46.0 m. D) Interlaminated clay and ripple-laminated very fine sand; transition zone; Warley Hill Formation; well
Core photographs. Length of bar scale is 4 cm.  A)  Interlaminated very fin...
Published: 01 November 2000
Figure 6 Core photographs. Length of bar scale is 4 cm. A) Interlaminated very fine to fine sand and clay; transition zone to lower shoreface; Warley Hill Formation; well MSB13CC, 42.7 m. B) Well sorted medium sand with low-angle cross-stratification; upper shoreface; Tinker Formation; well
Series: Geological Society, London, Special Reports, Geological Society, London, Special Reports
Published: 01 January 1999
DOI: 10.1144/SR23.4
EISBN: 9781786202864
... hills on the basin margin ( c .180 m O.D.) to below sea level in the Thames Estuary. The earliest Thames deposits, the Pebble Gravel Formation consists of fragmentary gravels composed predominantly of local materials, particularly flint. The Thames is the largest drainage basin in Britain...
Journal Article
Published: 01 March 2011
Journal of Paleontology (2011) 85 (2): 271–278.
... to 42 million years ago, or latest Ypresian through early Lutetian time; Gradstein et al., 2004 ). The Congaree and Warley Hill Formations in South Carolina are among the few outcropping strata in the southeastern United States that are referable to the lower or middle Lutetian (calcareous...
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Journal Article
Published: 02 May 2019
Petroleum Geoscience (2020) 26 (2): 325–345.
... al . 2000 ), where the formation ranges from late Asbian to Pendleian age ( Fig. 2 ). The top of the formation coincides with the base of the Millstone Grit Group, locally represented by the turbidite succession of the Pendle Grit Member or fluvial sandstones of the Warley Wise Grit, both of late...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1967
AAPG Bulletin (1967) 51 (12): 2400–2429.
... Formations commonly cover older deposits as a mantle. They are in few places more than 50 ft thick (maximum 196 ft in old Delaware River channel near Cape May). A few clay layers are present. Beacon Hill Gravel .—Thin remnants of gravel are present on the higher hills in Ocean, Monmouth...
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Journal Article
Published: 01 May 2003
Journal of Paleontology (2003) 77 (3): 491–508.
.... Weches Formation, middle Eocene (Claiborne); Localities 38, 39, 40, 68 and USGS 13269 (near Locality 68); Leon and San Augustine Counties, Texas. Warley Hill and Castle Hayne Formations, North and South Carolina ( Cooke, 1959 ). Unspecified formation, middle Eocene, Florida (type of P. pentagonium...
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Passive-margin sequence-stratigraphic model interpreted for coastal-plain s...
Published: 01 November 2000
decreased relative to sea-level rise, rate of deposition decreased and flooding occurred. Predominantly fine-grained sediment of the Warley Hill Formation (sequence 2) was deposited during this time. Subsequent sea-level fall resulted in renewed clastic sedimentation and progradation of sands onto the shelf
Journal Article
Published: 01 December 2004
Environmental Geosciences (2004) 11 (4): 205–220.
... they are primarily limestone ( Colquhoun et al., 1983 ; Harris et al., 1990 , 1993 ). The updip portion of the Congaree in the study area represents lower shoreface and inner bay and lagoonal deposits. The Warley Hill Formation unconformably overlies the Congaree Formation and consists of approximately 15 ft...
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Journal Article
Published: 06 September 2017
Geological Magazine (2018) 155 (8): 1742–1760.
...GENGO TANAKA; YASUHISA HENMI; TOSHIFUMI KOMATSU; KOJI HIROSE; HIROAKI UGAI; SHIGEHIRO KAWANO; HARUYOSHI MAEDA Abstract – The genus Neomonoceratina , which dominated the ostracod assemblage in the uppermost part of the Akasaki Formation (Miroku Group) of the Kyushu Island, Japan, is associated...
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Journal Article
Published: 02 April 2020
Petroleum Geoscience (2020) 26 (2): 303–324.
..., the most notable of which are the (Pendleian E1–E2a) Pendleton (or Pendle Grit) Formation, Warley Grit, Sabden Shale, Kinderscout Grit, Middle Grit and Rough Rock. Their recognition across the region suggests that basin subsidence was more uniform by Namurian times. Upper Carboniferous deposition...
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Journal Article
Published: 27 April 2020
Proceedings of the Yorkshire Geological Society (2020) 63 (1): 1–32.
... but of which much still remains to be learned. This review considers the relevance of these publications to our understanding of the sedimentology of Carboniferous strata, the geometries of Carboniferous basins, how these basins constrained the formation of reefs and controlled the movement of rivers...
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Journal Article
Published: 01 December 2004
Environmental Geosciences (2004) 11 (4): 181–190.
... and clay. Glauconite and microfossil assemblages indicate that the Fourmile formation is a shallow-marine deposit. The middle Eocene sediments include, in ascending order, the Congaree, Warley Hill, and Tinker and Santee formations. These units consist of alternating layers of sand, muddy and sandy...
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Journal Article
Published: 01 February 1995
Journal of the Geological Society (1995) 152 (1): 131–140.
...: Lithobionts in the Franz Joseph Springs at Badgeastein, Austria Mikroscopie 1985 42 124 134 Hill AS Hawkins S. J. An investigation of methods for sampling microbial films on rocky shores Journal of the Marine Biological Association 1990 70 77 88 Jeffree C.E. Read N.D...
Journal Article
Published: 29 May 2018
Petroleum Geoscience (2018) 24 (3): 287–322.
... Formation from the overlying Brennand Grit Formation (a correlative of the Warley Wise and Grassington Grit). The boundary between these formations is taken at the top of the Surgill Shale. It is equivalent to the Blacko Marine Band of the Clitheroe District ( Earp et al. 1961 ). Cores 20–28 (8480...
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Series: Geological Society, London, Special Reports
Published: 01 January 2016
DOI: 10.1144/SR27.14
EISBN: 9781862397071
... Depositional environment: Marine, outer neritic to upper bathyal. Subdivision: The most complete development of the Ormesby Clay Formation is in the Hales BH (Norfolk), where it was divided into four informal units (Knox et al . 1990) (Fig. 123 ): Unit OC1. Silty greyish brown...
Series: Geological Society, London, Geology of Series, Geological Society, London, Geology of Series
Published: 01 January 2006
DOI: 10.1144/GOEWP.9
EISBN: 9781862393882
... intrusion of the Whin Sill, a subsequent phase of east–west early Permian compression resulted in the formation of ESEtrending mineral veins associated with sinistral strike-slip movements ( Critchley 1984 ). North-trending structures include the reverse Dent Fault, forming the western margin of the Askrigg...
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Journal Article
Published: 01 March 2009
Environmental Geosciences (2009) 16 (1): 41–56.
... ), will be the focus of this article. The Congaree, Warley Hill, and Santee formations make up the Orangeburg Group, whereas the Barnwell Group consists of the Clinchfield, Dry Branch, and Tobacco Road Sand formations ( Jean et al., 2002 ). The Clinchfield Formation, a medium-grained, well-sorted, poorly...
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