Publication: [2734] The sedimentology of the Neoproterozoic Grampian Group and the significance of the Fort William Slide between Spean Bridge and Rubha Cuil-cheanna, Inverness-shire




Documented Paleocurrents


# Continental Area Stratigraphic Level Total Records Period Latitude Longitude Tectonic Plate Deposition Environment Paleocurrent Type Lithology Formation
1 Great Britain Proterozoic 4 11710 56.485 -10.1 Great Britain marine shallow crossbedding sandstone Fort William
2 Great Britain Proterozoic 4 11710 56.48 -5 Great Britain marine shallow crossbedding sandstone Fort William
3 Great Britain Proterozoic 4 11710 56.49 -10.1 Great Britain marine shallow crossbedding sandstone Fort William
4 Great Britain Proterozoic 4 11710 56.48 -10.1 Great Britain marine shallow crossbedding sandstone Fort William