The Lennoxtown essexite erratics train, central Scotland
This thesis is an investigation of glacial erratics derived from two small, adjacent, distinctive outcrops of essexlte near Lennoxtown, Central Scotland. Analysis of till samples has revealed that rock fragments and sand-size particles of essexite are absent up-ice of the essexite outcrops and scarc...
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University of Edinburgh
1977
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.661772 |