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Skip to Search Results- 12Jones, Brian
- 7Segger, Joachim
- 2Hunter, Ian G.
- 1Alonso Zarza, Ana M.
- 1Alonso-Zarza. Ana M.
- 1Beanish, Jennifer
- 11Earth and Atmospheric Sciences, Department of
- 10Earth and Atmospheric Sciences, Department of/Journal Articles (Earth and Atmospheric Sciences)
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- 7Music, Department of/Concert Programmes
- 1Earth and Atmospheric Sciences, Department of/Presentations (Earth and Atmospheric Sciences)
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1988-01-01
Paleontology is a multi-faceted subject that involves taxonomy and community analysis as two of its cornerstones. Both qualitative and quantitative approaches have been incorporated into the various methods employed in such analyses. Each paleontologist obvious has his or her own preference that...
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Desarrollo de calcretas en cavidades cársticas y/o de raíces: Las calcretes Cuaternarias de la Isla Gran Cayman (Calcrete development in root/karstic cavities: Quaternary calcretes from Grand Cayman)
Download1996-01-01
Alonso Zarza, Ana M., Jones, Brian
The ruggest karst terrain that is developed on the dolostones of the Miocene Caayman Formation on Grand Cayman includes numerous large cavities that formed through the activity of tree roots. The surfaces of those cavities are coated with laminated calcrete crusts that are up to 8 cm thick. These...
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Dynamic carbonate sedimentation in a shallow coastal lagoon: Case study of South Sound, Grand Cayman, British West Indies
Download2002-01-01
Beanish, Jennifer, Jones, Brian
South Sound is a 3.4 km-, shallow (.: 2 m), funnel-shaped lagoon located on the southwest exposed windward margin of Grand Cayman. The composition and distribution of the Thalassia, Sand, Rock Bottom, Brown Algae, Rubble, and Coral Head facies, are controlled by the dynamic interplay between...
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Marine-planation terraces on the shelf around Grand Cayman: a result of stepped Holocene sea-level rise
Download1995-01-01
The shelf around Grand Cayman consists of two seaward-sloping terraces separated by a mid-shelf scarp . Except along the exposed windward margin where coral growth is dominant, the upper terrace (0-10 m bal) largely consists of a barren rocky pavement traversed by erosional furrows. Exposure...
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2008-01-01
Jones, Brian, de Ronde, C., Renaut, Robin W.
The Giggenbach submarine volcano, which forms part of the Kermadec active arc front, is located ∼780 km NNE of the North Island of New Zealand. Samples collected from chimneys associated with seafloor hydrothermal vents on this volcano, at a depth of 160–180 m, contain silicified microbes and...