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The Geology of Moncreiffe Hill, Perthshire

Published online by Cambridge University Press:  01 May 2009

Charles F. Davidson
Affiliation:
University College, Dundee.

Extract

MONCREIFFE Hill, Perthshire, is the inclusive name for the series of low hills which form the uplands to the south and south-east of the City of Perth, and whose heather and grasscovered slopes reach in the summit of Moncreiffe Hill proper, a height of 725 feet above sea-level. The alluvium of the River Tay forms the northern boundary of the area under consideration, while on the east and south-east the hills are bounded by a continuation of the northern of the two faults which let down the Upper Old Red Sandstone outlier of the Carse of Gowrie, and by the Carse and Arctic clays of the River Earn. To the east of the City of Perth the area is bounded by the Lower Old Red Sandstone.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1932

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References

REFERENCES

(1)Ami, Boué., Essai géologique sur l’Écosse, Paris, 1820 (?), 142.Google Scholar
(2)Hickling, G.. “ The Old Red Sandstone of Forfarshire ”: Geol. Mag., 1908, 396.CrossRefGoogle Scholar
(3)Campbell, R.. “ The Geology of South-Eastern Kincardineshire ”: Trans. Roy. Soc. Edin., xlviii, iv, 1913, 923.CrossRefGoogle Scholar
(4)Allan, D. A.. “ The Geology of the Highland Border from Tayside to Noranside ”: Trans. Roy. Soc. Edin., lvi, i, 1928, 57.Google Scholar
(5)Sir Archibald, Geikie., Ancient Volcanoes of Great Britain, ii, 1897.Google Scholar
(6)Macnair, P.. The Geology and Scenery of the Grampian Mountains, ii, 1908.Google Scholar
(7)(Sir) Flett, J. S.. “ A Hypersthene Andesite from Dumyat ”: Trans. Geol. Soc. Edin., vii, 1897, 290.CrossRefGoogle Scholar
(8)Balsillie, D.. “ Note on a Hypersthene Andesite from Pitculla, Fifeshire ”: Geol. Mag., 1918, 346.CrossRefGoogle Scholar
(9)Fenner, C. N.. “ The Residual Liquids of Crystallising Magmas ”: Min. Mag., 1931, 539.Google Scholar
(10)Walker, F.. “ A Tholeiitic Phase of the Quartz-Dolerite Magma of Central Scotland ”: Min. Mag., 1930, 368.Google Scholar
(11)Walker, F. and Irving, J.. “ The Igneous Intrusions between St. Andrews and Loch Leven ”: Trans. Roy. Soc. Edin., lvi, i, 1928,12.Google Scholar
(12)Thomas, H. H. and Bailey, E. B., inThe Tertiary Geology of Mull, Loch Aline, and Oban ”: Mem. Geol. Surv., 1924, 136.Google Scholar
(13)Thomas, H. H., inThe Geology of Ardnamurchan, N. W. Mull, and Coll”: Mem. Geol. Surv., 1930, 114.Google Scholar
(14)Bailey, E. B., inThe Pre-Tertiary Geology of Mull, Loch Aline, and Oban”: Mem. Geol. Surv., 1925, 114.Google Scholar
(15)Bailey, E. B., inThe Geology of Ben Nevis and Glen Coe”: Mem. Geol. Surv., Sheet 53, 1916.Google Scholar
(16)Walker, F.. “ The Igneous Geology of Ardsheal Hill, ArgyllshireTrans. Roy. Soc. Edin., lv, 1922, 147.Google Scholar
(17)Harris, J. W.. “ The Extrusive Rocks of The Dundee District ”: Trans. Geol. Soc. Edin., xii, i, 1927.Google Scholar
(18)(Sir) Flett, J. S. and Seymour, H. J., inThe Geology of East Fife ”: Mem. Geol. Surv., 1902, 386.Google Scholar
(19)Jowett, A.. “ The Volcanic Rocks of the Forfarshire Coast ”: Quart. Journ. Geol. Soc., lxix, 1913, 459.CrossRefGoogle Scholar