Hostname: page-component-6d856f89d9-72csx Total loading time: 0 Render date: 2024-07-16T08:16:58.401Z Has data issue: false hasContentIssue false
  • English
  • Français

The Igneous Rocks of the Stanner-Hanter District, Radnorshire

Published online by Cambridge University Press:  01 May 2009

Norman Holgate  and
K. A. Knight Hallowes
Get access Rights & Permissions [Opens in a new window]

Extract

The igneous rocks of the Stanner-Hanter district are included within the Geological Survey I-inch map, sheet 56 S.E., (Old Series), and form three hog-backed hills, Stanner Rocks, Worsell Wood, and Hanter Hill, which are prominent features in the country between New Radnor and Kington, close to the Welsh border. This line of hills trends from south-west to north-east, though the separate ridges are arranged en échelon. Stanner Rocks (I,08I feet), is separated from Worsell Wrood (about 940 feet), by the alluvial plain of the Gilwern Brook, while there is a low col between Worsell Wood and Hanter Hill (I,36I feet).

Type
Articles
Information
Geological Magazine , Volume 78 , Issue 4 , August 1941 , pp. 241 - 267
Copyright
Copyright © Cambridge University Press 1941

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

IV. LIST OF WORKS TO WHICH REFERENCES IS MADE

Callaway, C., 1879. The Pre-Cambrian Rocks of Shropshire, Part I. Quart. Journ. Geol. Soc., xxxv, 644, 660.Google Scholar
Callaway, C., 1900. On Longmyndian Inliers at Old Radnor and Huntley (Gloucestershire). Quart. Journ. Geol. Soc., lvi, 511–520.CrossRefGoogle Scholar
Cobbold, E. S., and Whittard, W. F., 1935. The Helmeth Grits. Proc. Geol. Assoc, xlvi, 348.Google Scholar
Cole, G. A. J., 1886. The Igneous Rocks of Stanner. Geol. Mag., xxiii, 219.CrossRefGoogle Scholar
Garwood, E. J., and Goodyear, E., 1918. On the Geology of the Old Radnor District.Quart. Journ. Geol. Soc., lxxiv, 1–30.CrossRefGoogle Scholar
MacGregor, A. G., 1931. Clouded Felspars and Thermal Metamorphism. Min. Mag., xxii, 524–538.Google Scholar
Murchison, Sir R. I., 1838. The Silurian System, 318.Google Scholar
Murchison, Sir R. I., 1867. Siluria, 108, 109.Google Scholar
Nockolds, S. R., 1935. Contributions to the Petrology of Barnavave, I.F.S.I: The Junction Hybrids. Geol. Mag., Ixxii, 303.Google Scholar
Pocock, R. W., and Whitehead, T. H., 1935. British Regional Geology: The Welsh Borderland. H.M. Geological Survey and Museum, London, 72–3Google Scholar
Raw, F., 1904. Notes on the Igneous Intrusions of Stanner Rocks and Hanter Hill. Proc. Geol. Assoc, xviii, 460–2.CrossRefGoogle Scholar
Roberts, R. O., 1927. The Igneous and Associated Ordovician Rocks of Baxter's Bank, Radnorshire. Geol. Mag., lxiv, 289–298.CrossRefGoogle Scholar
Smith, H. G., 1918. The Basic Intrusions East of Gelli Hill, Radnorshire, Geol. Mag., lv, 500–7.CrossRefGoogle Scholar
Stamp, L. D., and Wooldridge, S. W., 1923. The Igneous and Associated Rocks of Llanwrtyd (Brecon). Quart. Journ. Geol. Soc, lxxix, 34–7, 42.Google Scholar
Watts, W. W., 1906. On the Igneous Rocks of the Welsh Border. Proc Geol. Assoc., xix, 178–180.Google Scholar
Winchell, A. N., 1933. Elements of Optical Mineralogy, Part II, 3rd edn., New York, 304.Google Scholar