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—Permeability profiles (parallel to paleocurrent) for Hayburn Wyke (small spacing) locality (Figure 7). At this close spacing, one can recognize correlatable subintervals with similar permeabilities. Solid black lines outline these subintervals, which have horizontal extents of 0.5–2.7 m (minimum value). K = permeability.

—Permeability profiles (parallel to paleocurrent) for Hayburn Wyke (small s... Available to Purchase

Published: 01 April 1990
Figure 12 —Permeability profiles (parallel to paleocurrent) for Hayburn Wyke (small spacing) locality ( Figure 7 ). At this close spacing, one can recognize correlatable subintervals with similar permeabilities. Solid black lines outline these subintervals, which have horizontal extents of 0.5
Journal Article

First record of the pterosaur footprint Pteraichnus from the Saltwick Formation (Aalenian) of the Cleveland Basin, Yorkshire, UK Available to Purchase

M. A. Whyte, M. Romano
Published: 29 April 2014
Proceedings of the Yorkshire Geological Society (2014) 60 (1): 19–27.
DOI: https://doi.org/10.1144/pygs2014-338
...M. A. Whyte; M. Romano Summary Prints belonging to Pteraichnus are recorded and described from the Saltwick Formation (Middle Jurassic, Aalenian Stage) at Hayburn Wyke on the Cleveland Coast of Yorkshire, England. This is the first record of Pteraichnus from the region and from the British Isles...
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—Plot of permeability ranges for the six main facies in the active fill of the ribbon-like distributary channel sand bodies. Data for the Hayburn Wyke (A–C), Burniston Wyke (D), and Whitby (E) localities are plotted separately. Facies codes are explained in Table 1. K = permeability.

—Plot of permeability ranges for the six main facies in the active fill of ... Available to Purchase

Published: 01 April 1990
Figure 8 —Plot of permeability ranges for the six main facies in the active fill of the ribbon-like distributary channel sand bodies. Data for the Hayburn Wyke (A–C), Burniston Wyke (D), and Whitby (E) localities are plotted separately. Facies codes are explained in Table 1 . K = permeability.
Image
Lithological log of the upper Saltwick Formation and lower Eller Beck Formation at Hayburn Wyke [TA 0117 9690]. Probable horizon from which the block containing the tracks of Pteraichnus occur is indicated. est. = estimated; n.e. = no exposure.

Lithological log of the upper Saltwick Formation and lower Eller Beck Forma... Available to Purchase

Published: 29 April 2014
Fig. 2. Lithological log of the upper Saltwick Formation and lower Eller Beck Formation at Hayburn Wyke [TA 0117 9690]. Probable horizon from which the block containing the tracks of Pteraichnus occur is indicated. est. = estimated; n.e. = no exposure.
Image
—Map of the study area on the eastern coast of Yorkshire, England. Localities where the minipermeameter was applied are marked by black squares. S, M, and L refer to the three different measurement spacings (small, medium, and large, respectively; see Table 1) used at Hayburn Wyke.

—Map of the study area on the eastern coast of Yorkshire, England. Localiti... Available to Purchase

Published: 01 April 1990
Figure 7 —Map of the study area on the eastern coast of Yorkshire, England. Localities where the minipermeameter was applied are marked by black squares. S, M, and L refer to the three different measurement spacings (small, medium, and large, respectively; see Table 1 ) used at Hayburn Wyke.
Image
Summary graphic log of the Ravenscar Group, NE Yorkshire coast, made up from sections at Blea Wyke, from Hayburn Wyke to Burniston Bay, and at Cayton Bay and Gristhorpe Bay. (Full details of the succession are given in fig. 7. Sample locations can be obtained from The Journal of Geology's Data Depository.) Heights are based on our own field measurements, supplemented by data from the Ravenscar borehole, which were used to give total thickness of the Saltwick, Cloughton, and Scalby Formations (Eschard et al. 1991). M=marine units, within an otherwise nonmarine sequence. L.M.=Lebberston  Member; M.G.M.=Moor  Grit Member. Refer to tables 1 and 2 for stomatal density data. The stomatal density data of McElwain (1997) are based on examination of Harris’s collection in the Natural History Museum, London, and because this collection is not precisely located stratigraphically, large vertical error bars are shown (relevant data enclosed by balloons). Stomatal density work carried out for this study relies on material collected from specific plant beds: H=Hayburn Wyke Plant Bed; E=Negative Excursion Horizon; S=Solenites Bed. Other well-known plant beds are shown in figure 7. Approximate numeric ages from the Pálfy et al. (2000) timescale. The Cornbrash, at ∼196 m in the section, is a condensed limestone, and close juxtaposition of fossils of different ages probably explains the spread of carbon-isotope values within the unit.

Summary graphic log of the Ravenscar Group, NE Yorkshire coast, made up fro... Available to Purchase

Published: 01 May 2003
Figure 2. Summary graphic log of the Ravenscar Group, NE Yorkshire coast, made up from sections at Blea Wyke, from Hayburn Wyke to Burniston Bay, and at Cayton Bay and Gristhorpe Bay. (Full details of the succession are given in fig. 7 . Sample locations can be obtained from The Journal
Image
Transverse section through a composite crevasse-splay succession in the lower part of the Saltwick Formation, Hayburn Wyke, Yorkshire (modified from Mjøs et al. 1993). The splays are confined in their axial part (LOC F-H) but display discrete sheets laterally. Throughout, the splay complex is finer grained than a contemporaneous channel to the south (LOC A). Numbers refer to depositional elements 7–18 in Figure 28.

Transverse section through a composite crevasse-splay succession in the low... Available to Purchase

Published: 28 October 2019
Fig. 29.— Transverse section through a composite crevasse-splay succession in the lower part of the Saltwick Formation, Hayburn Wyke, Yorkshire (modified from Mjøs et al. 1993 ). The splays are confined in their axial part (LOC F-H) but display discrete sheets laterally. Throughout, the splay
Image
Detailed graphic log of the Ravenscar Group along a 4-km stretch of coast between Hayburn Wyke and Burniston Wyke, NE Yorkshire, England. From 21 to 33.5 m at TA012969; from 37 to 61 m at TA016968 to TA018963; from 67 to 86 m at TA020959 to TA021955 (this part of the succession shows great lateral variability); from 86 to 106.3 m at TA021955 to TA020951; from 106.3 to 133.9 m at TA020951 to TA026949; from 133.9 to 144.5 m at TA026949 to TA027947; from 144.5 to 160.4 m at TA028943 to TA028932. (Locations use the standard Ordnance Survey grid reference.) The major plant beds of Black (1929), Harris (1961, 1964, 1969, 1979), and Harris et al. (1974) are indicated. Vertical boxes between 54.5 and 55.5 m, 56.5 and 58.5 m, and at about 71 m indicate where samples were taken in cases of significant lateral facies variability. WNIM=White  Nab Ironstone Member; BGM=Blow  Gill Member.

Detailed graphic log of the Ravenscar Group along a 4-km stretch of coast b... Available to Purchase

Published: 01 May 2003
Figure 7. Detailed graphic log of the Ravenscar Group along a 4-km stretch of coast between Hayburn Wyke and Burniston Wyke, NE Yorkshire, England. From 21 to 33.5 m at TA012969; from 37 to 61 m at TA016968 to TA018963; from 67 to 86 m at TA020959 to TA021955 (this part of the succession shows
Image
Detailed graphic log of the Ravenscar Group along a 4-km stretch of coast between Hayburn Wyke and Burniston Wyke, NE Yorkshire, England. From 21 to 33.5 m at TA012969; from 37 to 61 m at TA016968 to TA018963; from 67 to 86 m at TA020959 to TA021955 (this part of the succession shows great lateral variability); from 86 to 106.3 m at TA021955 to TA020951; from 106.3 to 133.9 m at TA020951 to TA026949; from 133.9 to 144.5 m at TA026949 to TA027947; from 144.5 to 160.4 m at TA028943 to TA028932. (Locations use the standard Ordnance Survey grid reference.) The major plant beds of Black (1929), Harris (1961, 1964, 1969, 1979), and Harris et al. (1974) are indicated. Vertical boxes between 54.5 and 55.5 m, 56.5 and 58.5 m, and at about 71 m indicate where samples were taken in cases of significant lateral facies variability. WNIM=White  Nab Ironstone Member; BGM=Blow  Gill Member.

Detailed graphic log of the Ravenscar Group along a 4-km stretch of coast b... Available to Purchase

Published: 01 May 2003
Figure 7. Detailed graphic log of the Ravenscar Group along a 4-km stretch of coast between Hayburn Wyke and Burniston Wyke, NE Yorkshire, England. From 21 to 33.5 m at TA012969; from 37 to 61 m at TA016968 to TA018963; from 67 to 86 m at TA020959 to TA021955 (this part of the succession shows
Image
Examples of the fine-grained channel, and overbank Facies Associations. (a) Mudstone-dominated channel deposits (FA3) associated with FA2 exposed north of Long Nab in the Scalby Formation. The main channel fill deposit is mudstone with an occasional thin lenticular fine-grained sandstone layer. (b) Small ribbon-shaped crevasse channel with extended splay sheet sandstone from the Saltwick Formation exposed at High Whitby. (c) Coarsening-upward splay complex deposits at Cloughton Wyke in the Gristhorpe Member and detailed sedimentology of interdistributary bay-fill splay complex with tidal sedimentary structures, cut and fill nature and traces of rooting. (d) Fining-upward heterolithic levee deposits on the top of the older channel bar deposits at Whitby West Cliff in the Saltwick Formation. (e) Shallow lake or ponded floodplain mudstone deposits at the South of Long Nab in the Long Nab Member. (f) Grey massive floodplain mudstone deposits at Whitby West Cliff in the Saltwick Formation. (g) Mottled palaeosol at Burniston Bay in the Long Nab Member. (h) Partial soil development in the coastal swamp deposits exposed at North of Hayburn Wyke in the lower part of the Saltwick Formation.

Examples of the fine-grained channel, and overbank Facies Associations. ( a... Open Access

Published: 08 April 2022
in the Long Nab Member. ( f ) Grey massive floodplain mudstone deposits at Whitby West Cliff in the Saltwick Formation. ( g ) Mottled palaeosol at Burniston Bay in the Long Nab Member. ( h ) Partial soil development in the coastal swamp deposits exposed at North of Hayburn Wyke in the lower part
Journal Article

Minipermeameter-Based Study of Permeability Trends in Channel Sand Bodies Available to Purchase

T. Dreyer, Å. Scheie, O. Walderhaug
Journal: AAPG Bulletin
Published: 01 April 1990
AAPG Bulletin (1990) 74 (4): 359–374.
DOI: https://doi.org/10.1306/0C9B22F9-1710-11D7-8645000102C1865D
...Figure 12 —Permeability profiles (parallel to paleocurrent) for Hayburn Wyke (small spacing) locality ( Figure 7 ). At this close spacing, one can recognize correlatable subintervals with similar permeabilities. Solid black lines outline these subintervals, which have horizontal extents of 0.5...
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Notes on new xiphosurid (horseshoe crab) trackways from the Middle Jurassic of the Cleveland Basin, Yorkshire, UK Available to Purchase

Mike Romano, Robert Taylor
Published: 21 September 2016
Proceedings of the Yorkshire Geological Society (2016) 61 (2): 155–160.
DOI: https://doi.org/10.1144/pygs2016-376
... and by a single part, were found loose by one of us (RT) on the foreshore between Ravenscar and Hayburn Wyke, below Beast Cliff, c. 12.5 km SE of Whitby ( Fig. 1 ). The cliffs along this stretch of coast comprise much of the Ravenscar Group, and the loose specimens could have come from any one of the Saltwick...
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Journal Article

Carbon-Cycle Perturbation in the Middle Jurassic and Accompanying Changes in the Terrestrial Paleoenvironment Available to Purchase

Stephen P. Hesselbo, Helen S. Morgans-Bell, Jennifer C. McElwain, P. McAllister Rees, Stuart A. Robinson, C. Elizabeth Ross
Published: 01 May 2003
The Journal of Geology (2003) 111 (3): 259–276.
DOI: https://doi.org/10.1086/373968
...Figure 2. Summary graphic log of the Ravenscar Group, NE Yorkshire coast, made up from sections at Blea Wyke, from Hayburn Wyke to Burniston Bay, and at Cayton Bay and Gristhorpe Bay. (Full details of the succession are given in fig. 7 . Sample locations can be obtained from The Journal...
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Journal Article

Two previously unrecorded xiphosurid trace fossils, Selenichnites rossendalensis and Crescentichnus tesiltus , from the Middle Jurassic of Yorkshire, UK Available to Purchase

Mike Romano, Robert Taylor
Published: 28 February 2019
Proceedings of the Yorkshire Geological Society (2019) 62 (4): 254–259.
DOI: https://doi.org/10.1144/pygs2018-017
... on an estimate from the width of the appendage imprints of the trackway. Recently one of us (RT) found a single specimen, here assigned to S . cf. hundalensis from the Saltwick Formation in Hayburn Wyke, 2 km north of Cloughton Wyke, though the source horizon could not be located. This specimen...
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View PDF for article title, Two previously unrecorded xiphosurid trace fossils, Selenichnites rossendalensis and Crescentichnus tesiltus , from the Middle Jurassic of Yorkshire, UK
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Journal Article

Virtual outcrop-based analysis of channel and crevasse splay sandstone body architecture in the Middle Jurassic Ravenscar Group, Yorkshire, NE England Open Access

M. Mostafizur Rahman, John A. Howell, David I. M. Macdonald
Published: 08 April 2022
Journal of the Geological Society (2022) 179 (3): jgs2021-017.
DOI: https://doi.org/10.1144/jgs2021-017
... in the Long Nab Member. ( f ) Grey massive floodplain mudstone deposits at Whitby West Cliff in the Saltwick Formation. ( g ) Mottled palaeosol at Burniston Bay in the Long Nab Member. ( h ) Partial soil development in the coastal swamp deposits exposed at North of Hayburn Wyke in the lower part...
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View PDF for article title, Virtual outcrop-based analysis of channel and crevasse splay sandstone body architecture in the Middle Jurassic Ravenscar Group, Yorkshire, NE England
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Journal Article

Behavioural variation in limulids (Xiphosurida) from the Middle Jurassic of the Cleveland Basin, Yorkshire, UK, as deduced from their traces: a review and reappraisal Available to Purchase

Mike Romano
Published: 07 August 2020
Proceedings of the Yorkshire Geological Society (2021) 63 (3): pygs2020-005.
DOI: https://doi.org/10.1144/pygs2020-005
... : Cloughton Wyke) C. tesiltus 60 mm ( Romano and Taylor 2019 : Cloughton Wyke) C. isp. indet . 90 mm (Taylor photograph 6/5/19: Cloughton) C. isp. indet . 80 mm (Taylor photograph 6/5/19: Cloughton) Saltwick Formation: S. hundalensis 66 mm (Taylor photograph 27/8/18: Hayburn) K...
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Jurassic sedimentation in the Cleveland Basin: a review Available to Purchase

J. H. Powell
Published: 01 May 2010
Proceedings of the Yorkshire Geological Society (2010) 58 (1): 21–72.
DOI: https://doi.org/10.1144/pygs.58.1.278
... of Ginkgo alone ( Harris 1953 ). Plants rapidly colonized the substrate and stabilized the interfluves, resulting in high sinuosity and meandering channels. Classic localities at Hayburn Wyke, Cloughton Wyke and Whitby are famous for the preservation of drifted plants deposited in shallow, freshwater pools...
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Jurassic dinosaur tracks and trackways of the Cleveland Basin, Yorkshire: preservation, diversity and distribution Available to Purchase

M. Romano, M. A. Whyte
Published: 01 May 2003
Proceedings of the Yorkshire Geological Society (2003) 54 (3): 185–215.
DOI: https://doi.org/10.1144/pygs.54.3.185
... Group of the Cleveland Basin ranges in age from the early Aalenian to late Bathonian ( Fig. 3 ). The Aalenian/Bajocian boundary is not well defined, but the above authors assigned the Saltwick (=Hayburn) and Eller Beck formations to the Aalenian, and the base of the Bajocian is tentatively placed...
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“Grain-size bookkeeping,” a new aid for siliciclastic systems with examples from paralic environments Available to Purchase

Tony Reynolds
Published: 28 October 2019
Journal of Sedimentary Research (2019) 89 (10): 976–1016.
DOI: https://doi.org/10.2110/jsr.2019.53
...Fig. 29.— Transverse section through a composite crevasse-splay succession in the lower part of the Saltwick Formation, Hayburn Wyke, Yorkshire (modified from Mjøs et al. 1993 ). The splays are confined in their axial part (LOC F-H) but display discrete sheets laterally. Throughout, the splay...
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