Mapwork based on Ordnance Survey Licence number[removed]Fidra and Lamb can be seen farther to the west. They are part of another intrusion forming a sheet of basalt rock called a sill. Craigleith is lower with sloping - Craigleith - Document - PDFSEARCH.IO

First Page	Meta Content
	Mapwork based on Ordnance Survey Licence number[removed]Fidra and Lamb can be seen farther to the west. They are part of another intrusion forming a sheet of basalt rock called a sill. Craigleith is lower with sloping Add to Reading List Document Date: 2010-11-11 04:11:21 Open Document File Size: 453,87 KB Share Result on Facebook City Edinburgh / / Company Borders RIGS Group / / Country Scotland / Iceland / Iceland and Hawaii / / / Event Natural Disaster / / Facility North Berwick harbour / Seabird Centre / North Berwick pier / Scottish Seabird Centre / University of Edinburgh / / IndustryTerm car parks / chemicals / car park / / NaturalFeature Lamb Island / / Organization Edinburgh Geological Society / University of Edinburgh / Scottish Seabird Centre / / Person Ash Green Volcanic Ash Volcanic / Angus Miller / Colin Souness / Neil van Beinum / Ash Volcanic Vent Agglomerate Basalt / Derek Munn / / / ProvinceOrState Hawaii / / URL www.edinburghgeolsoc.org / www.traveline.org.uk / / SocialTag Volcanology Volcanic rocks Igneous rocks Plate tectonics Lava Basalt Volcano Agglomerate Tuff Geology

Mapwork based on Ordnance Survey Licence number[removed]Fidra and Lamb can be seen farther to the west. They are part of another intrusion forming a sheet of basalt rock called a sill. Craigleith is lower with slopingAdd to Reading List