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Staple Newk

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Journal Article
Published: 01 November 2008
Proceedings of the Yorkshire Geological Society (2008) 57 (2): 95–106.
...I. C. Starmer Summary At Staple Newk [TA 205 737], intensive folding and thrusting of the Chalk were restricted to a 200 m long section. The ENE-WSW folding and NNW-SSE thrusting resulted from dextral transpressive reactivation of the underlying ENE-WSW Bempton Fault. Detachment folding...
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<span class="search-highlight">Staple</span> <span class="search-highlight">Newk</span> cliffs. (Note the orientation differs slightly from that of  Fi...
Published: 01 November 2008
Fig 2. Staple Newk cliffs. (Note the orientation differs slightly from that of Fig. 3 .)
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<span class="search-highlight">Staple</span> <span class="search-highlight">Newk</span>: vertical section and map. (Note the orientation differs slight...
Published: 01 November 2008
Fig. 3. Staple Newk: vertical section and map. (Note the orientation differs slightly from that of Fig. 2 .)
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Evolution of the <span class="search-highlight">Staple</span> <span class="search-highlight">Newk</span> structures.
Published: 01 November 2008
Fig. 5. Evolution of the Staple Newk structures.
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A boat trip led by the author in June 2015 for the Yorkshire Midweek Geolog...
Published: 21 August 2020
Fig. 9. A boat trip led by the author in June 2015 for the Yorkshire Midweek Geology Group approaching Staple Newk and the section of deformed chalk.
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Front cover of the  Proceedings of the Yorkshire Geological Society  showin...
Published: 21 August 2020
Fig. 8. Front cover of the Proceedings of the Yorkshire Geological Society showing J.W. Davis 1885 party on the shore below the contortions in the chalk cliffs at Staple Newk (reproduced from the Proceedings of the Yorkshire Geological Society , 50 , part 3, by permission of the Council
Journal Article
Published: 01 May 2013
Proceedings of the Yorkshire Geological Society (2013) 59 (3): 195–201.
... to isolated, gentle E–W folds and E–W zones of localized intense deformation at Staple Newk and Selwicks Bay that are related to reactivations of the E-W Fault Belt. Starmer (1995) suggested that the north–south extension complex at Selwicks Bay formed a hinge for the southward regional tilt of the area...
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Journal Article
Published: 21 August 2020
Proceedings of the Yorkshire Geological Society (2020) 63 (2): 147–161.
...Fig. 9. A boat trip led by the author in June 2015 for the Yorkshire Midweek Geology Group approaching Staple Newk and the section of deformed chalk. ...
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Journal Article
Published: 09 August 2018
Proceedings of the Yorkshire Geological Society (2019) 62 (3): 153–177.
... Society , 50 , 213 – 228 , https://doi.org/10.1144/pygs.50.3.213 Starmer , I.C. 2008 . The concentration of folding and faulting in the Chalk at Staple Newk (Scale Nab) near Flamborough, East Yorkshire . Proceedings of the Yorkshire Geological Society , 57 , 95 – 106 , https://doi.org...
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Journal Article
Published: 01 November 2009
Proceedings of the Yorkshire Geological Society (2009) 57 (3-4): 193–216.
... and the North Sea Basin . Proceedings of the Yorkshire Geological Society , 50 , 213 – 228 . Starmer , I. C. 2008 . The concentration of folding and faulting in the Chalk at Staple Newk (Scale Nab) near Flamborough, East Yorkshire . Proceedings of the Yorkshire Geological Society , 57 , 95...
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Journal Article
Published: 06 December 2021
Proceedings of the Yorkshire Geological Society (2022) 64 (1): pygs2021-008.
... Rambles in East Yorkshire . Brown & Sons , London . Smith , W. 1815 . A Memoir to the Map and Delineation of the Strata of England and Wales, with A Part of Scotland . John Cary , London . Starmer , I.C . 2008 . The concentration of folding and faulting in the Chalk at Staple...
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