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ISSN 0016-7649
EISSN 2041-479X
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Journal of the Geological Society November 01, 2017, Vol.174, 953. doi:10.1144/jgs2017-Awa

Research Article

Journal of the Geological Society July 11, 2017, Vol.174, 954-967. doi:10.1144/jgs2017-008
Journal of the Geological Society June 05, 2017, Vol.174, 968-978. doi:10.1144/jgs2017-010
Journal of the Geological Society July 11, 2017, Vol.174, 979-987. doi:10.1144/jgs2017-011
Journal of the Geological Society September 15, 2017, Vol.174, 988-1003. doi:10.1144/jgs2017-001
Journal of the Geological Society June 05, 2017, Vol.174, 1004-1018. doi:10.1144/jgs2016-159
Journal of the Geological Society June 29, 2017, Vol.174, 1019-1030. doi:10.1144/jgs2017-022
Journal of the Geological Society July 11, 2017, Vol.174, 1031-1047. doi:10.1144/jgs2016-133
Journal of the Geological Society June 05, 2017, Vol.174, 1048-1061. doi:10.1144/jgs2017-013
Journal of the Geological Society June 29, 2017, Vol.174, 1062-1069. doi:10.1144/jgs2017-051
Journal of the Geological Society July 11, 2017, Vol.174, 1070-1089. doi:10.1144/jgs2017-007
Journal of the Geological Society June 06, 2017, Vol.174, 1090-1112. doi:10.1144/jgs2016-127
  • Cover Image

    Cover Image

    issue cover

    Cover image: The photo shows a clock-wise 90° rotation of a cross-stratified Navajo Sandstone at a location known as “The Wave”. The wave outcrops in Coyote Buttes North, part of the Paria Canyon/Vermillion Cliffs wilderness on the borders of Utah and Arizona in USA. The rocks are coloured red by iron oxide which picks out subtle changes in grainsize due to deposition on desert sand dunes that were active in the Jurassic. The large scale sets of cross-strata in the Navajo Sandstone have been sculpted by wind and water to create the flowing shapes of the wave.

    Photo: Charlie Bristow

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