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ISSN 0016-7649
EISSN 2041-479X
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Journal of the Geological Society March 07, 2017, Vol.174, 609-626. doi:10.1144/jgs2016-101
Journal of the Geological Society March 21, 2017, Vol.174, 627-645. doi:10.1144/jgs2016-132
Journal of the Geological Society March 07, 2017, Vol.174, 646-654. doi:10.1144/jgs2016-043
Journal of the Geological Society March 07, 2017, Vol.174, 655-666. doi:10.1144/jgs2016-129
Journal of the Geological Society March 07, 2017, Vol.174, 667-678. doi:10.1144/jgs2016-107
Journal of the Geological Society February 23, 2017, Vol.174, 679-699. doi:10.1144/jgs2016-124
Journal of the Geological Society February 23, 2017, Vol.174, 701-720. doi:10.1144/jgs2016-097
Journal of the Geological Society February 23, 2017, Vol.174, 721-740. doi:10.1144/jgs2016-006
Journal of the Geological Society March 07, 2017, Vol.174, 741-758. doi:10.1144/jgs2016-130
Journal of the Geological Society March 21, 2017, Vol.174, 759-772. doi:10.1144/jgs2016-080
Journal of the Geological Society March 21, 2017, Vol.174, 773-786. doi:10.1144/jgs2016-105
Journal of the Geological Society March 21, 2017, Vol.174, 787-790. doi:10.1144/jgs2016-157
Journal of the Geological Society March 21, 2017, Vol.174, 791-792. doi:10.1144/jgs2017-016
  • 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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