File:P215702.jpg
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Summary
description | English: Boulder bed in the Port Askaig Tillite Formation, Argyll Group, Islay; cleaved and containing large clasts mainly of granite (C 1276). Figure 13 Geological sketch map and section of the Jura area—with along-strike stratigraphical section showing relationships at the end of Craignish Phyllite times (modified from Anderton, 1979; 1985). STF—Scarba Transfer Fault and ITF—Islay Transfer Fault are interpreted growth faults and do not crop out at the surface. Note that the sense of movement on the STF reverses after the deposition of the Jura Quartzite. Hence the thick accumulation of Jura Quartzite lies to the south of the fault, whereas the thick accumulation of Easdale Slate and Craignish Phyllite lies to the north. BD = Bonahaven Dolomite; PAT = Port Askaig Tillite. BGS image ID: P215702. |
source | British Geological Survey |
author | British Geological Survey |
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