Glen Ugie Peak
Glenugie Peak with eastern grey kangaroos (at bottom left)
|Elevation||316 m (1,037 ft)|
|Location||Northern Rivers region, New South Wales, Australia|
|Age of rock||Cenozoic|
Glenugie Peak, also known as Mount Elaine or as Glen Ugie Peak, a mountain that is part of the ridge surrounding the Clarence Moreton Basin, is situated in the Northern Rivers region of New South Wales, Australia. At an elevation of 316 metres (1,037 ft) above sea level, the mountain is located near the Pacific Highway, south of the town of Grafton and approximately 6 kilometres (3.7 mi) west north-west of the locality of Calamia.
Features and location
It is a dolerite peak from the Cenozoic era extruded from the Grafton Formation. The Grafton Formation is a series of sedimentary rocks, laid down between the late Jurassic and early Cretaceous periods.
Glenugie Peak is noted by Matthew Norman for its dry rainforest in a gully which includes a number of rare species of trees, as well as the Yellow Box, which is more often associated with areas west of the Great Dividing Range. Average annual rainfall is 1,138 millimetres (44.8 in).
- "Glenugie Peak". Geographical Names Register (GNR) of NSW. Geographical Names Board of New South Wales. Retrieved 13 May 2015.
- "Gumbaynggirr Language" (PDF).
- Floyd, A. G. (1989). Rainforest Trees of Mainland South-eastern Australia. Inkata Press. p. 76. ISBN 0-909605-57-2.
- "Secrets of a Basalt Hill". NSW Department of Industry and Investment.
- "29 Mar 1913 - GLENUGIE QUARRY. - Trove". Nla.gov.au. 1913-03-29. Retrieved 2016-02-25.
|This volcanology article is a stub. You can help Wikipedia by expanding it.|
|This article about a specific stratigraphic formation is a stub. You can help Wikipedia by expanding it.|
|This New South Wales geography article is a stub. You can help Wikipedia by expanding it.|