The igneous rocks of the Mountsorrel area, by reason of their accessibility and economic value, have attracted the attention of geologists since the middle of last century. The latest and most comprehensive account of the district is that of E. E. Lowe (1) and at the end of the paper a useful bibliography of earlier publications is given. Additional notes are to be found in the pamphlet published for the visit of the Geologists' Association to Charnwood Forest in 1928, including a structural study of the Mountsorrel “granite” by F. Jones (2).
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