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ISSN 0016-7649
EISSN 2041-479X
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Journal of the Geological Society May 03, 2017, Vol.174, 793-802. doi:10.1144/jgs2016-142
Journal of the Geological Society May 03, 2017, Vol.174, 803-816. doi:10.1144/jgs2016-152
Journal of the Geological Society May 15, 2017, Vol.174, 817-835. doi:10.1144/jgs2016-100
Journal of the Geological Society May 15, 2017, Vol.174, 836-849. doi:10.1144/jgs2016-119
Journal of the Geological Society May 15, 2017, Vol.174, 850-854. doi:10.1144/jgs2016-147
Journal of the Geological Society May 15, 2017, Vol.174, 855-868. doi:10.1144/jgs2016-122
Journal of the Geological Society April 17, 2017, Vol.174, 869-882. doi:10.1144/jgs2016-146
Journal of the Geological Society May 15, 2017, Vol.174, 883-891. doi:10.1144/jgs2017-005
Journal of the Geological Society May 15, 2017, Vol.174, 893-912. doi:10.1144/jgs2016-145
Journal of the Geological Society April 04, 2017, Vol.174, 913-928. doi:10.1144/jgs2016-155
Journal of the Geological Society May 15, 2017, Vol.174, 929-946. doi:10.1144/jgs2016-160
Journal of the Geological Society April 17, 2017, Vol.174, 947-950. doi:10.1144/jgs2017-004
Journal of the Geological Society April 28, 2017, Vol.174, 950-952. doi:10.1144/jgs2017-031
  • 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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