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Scotfot at 23:45, 16 December 2022

2022-12-16T23:45:38Z

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	== Summary ==		== Summary ==
	Table 4 Ammonite zonal sequence in the Lower Jurassic and part of the Middle Jurassic of the Inner Hebrides (based on Richey, 1961 and Cope, 1995).The correlation with the major lithostratigraphical divisions is based on Morton and Dietl (1989), Howarth (1992), Hesselbo et al. (1998), Morton (1999b), and Hesselbo and Coe (2000) with additional information from N Morton and J D Hudson, 2000 and 2004. Members are from the type area of the Bearreraig Sandstone Formation, in Trotternish, Skye. Localities: 1 Mull; 2 Morvern; 3 Ardnamurchan; 4 Skye; 5 Raasay; 6 Scalpay; 7 Shiant Isles; 8 Arran * developed only in south of district † in Skye, Upper Triassic to Hettangian (Morton and Hudson, 1995) – not recorded in district. From: Emeleus, C H, and Bell, B R. 2005. British regional geology: The Palaeogene volcanic districts of Scotland. Fourth edition. Keyworth, Nottingham: British Geological Survey.		Table 4 Ammonite zonal sequence in the Lower Jurassic and part of the Middle Jurassic of the Inner Hebrides (based on Richey, 1961 and Cope, 1995).The correlation with the major lithostratigraphical divisions is based on Morton and Dietl (1989), Howarth (1992), Hesselbo et al. (1998), Morton (1999b), and Hesselbo and Coe (2000) with additional information from N Morton and J D Hudson, 2000 and 2004. Members are from the type area of the Bearreraig Sandstone Formation, in Trotternish, Skye. Localities: 1 Mull; 2 Morvern; 3 Ardnamurchan; 4 Skye; 5 Raasay; 6 Scalpay; 7 Shiant Isles; 8 Arran * developed only in south of district † in Skye, Upper Triassic to Hettangian (Morton and Hudson, 1995) – not recorded in district. From: Emeleus, C H, and Bell, B R. 2005. British regional geology: The Palaeogene volcanic districts of Scotland. Fourth edition. Keyworth, Nottingham: British Geological Survey.

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Scotfot: Table 4 Ammonite zonal sequence in the Lower Jurassic and part of the Middle Jurassic of the Inner Hebrides (based on Richey, 1961 and Cope, 1995).The correlation with the major lithostratigraphical divisions is based on Morton and Dietl (1989), Howarth (1992), Hesselbo et al. (1998), Morton (1999b), and Hesselbo and Coe (2000) with additional information from N Morton and J D Hudson, 2000 and 2004. Members are from the type area of the Bearreraig Sandstone Formation, in Trotternish, Skye. Lo...

2022-12-16T23:44:57Z

Table 4 Ammonite zonal sequence in the Lower Jurassic and part of the Middle Jurassic of the Inner Hebrides (based on Richey, 1961 and Cope, 1995).The correlation with the major lithostratigraphical divisions is based on Morton and Dietl (1989), Howarth (1992), Hesselbo et al. (1998), Morton (1999b), and Hesselbo and Coe (2000) with additional information from N Morton and J D Hudson, 2000 and 2004. Members are from the type area of the Bearreraig Sandstone Formation, in Trotternish, Skye. Lo...

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== Summary ==
Table 4 Ammonite zonal sequence in the Lower Jurassic and part of the Middle Jurassic of the Inner Hebrides (based on Richey, 1961 and Cope, 1995).The correlation with the major lithostratigraphical divisions is based on Morton and Dietl (1989), Howarth (1992), Hesselbo et al. (1998), Morton (1999b), and Hesselbo and Coe (2000) with additional information from N Morton and J D Hudson, 2000 and 2004. Members are from the type area of the Bearreraig Sandstone Formation, in Trotternish, Skye. Localities: 1 Mull; 2 Morvern; 3 Ardnamurchan; 4 Skye; 5 Raasay; 6 Scalpay; 7 Shiant Isles; 8 Arran * developed only in south of district † in Skye, Upper Triassic to Hettangian (Morton and Hudson, 1995) – not recorded in district. From: Emeleus, C H, and Bell, B R. 2005. British regional geology: The Palaeogene volcanic districts of Scotland. Fourth edition. Keyworth, Nottingham: British Geological Survey.