Author:
Holgate Norman,Knight Hallowes K. A.
Abstract
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).
Publisher
Cambridge University Press (CUP)
Reference16 articles.
1. The Helmeth Grits;Cobbold;Proc. Geol. Assoc,1935
2. The Pre-Cambrian Rocks of Shropshire, Part I;Callaway;Quart. Journ. Geol. Soc.,1879
3. Clouded felspars and thermal metamorphism
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