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Roe Plains

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Origin of the Late Neogene Roe Plains and their calcarenite veneer: implications for sedimentology and tectonics in the Great Australian Bight
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Kendrick, George W; McNamara, Kenneth J; Brimmell, K; Western Australian Museum. Dept. of Earth and Planetary Sciences (1997),
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The Roe Plains are predominantly marine dunes on a coastal plain. The plains are bounded on the south by the
48: 236: 128: 138:. Similar to the caves of the Hampton Tableland, the Roe Plains have a resource of fossil deposits. 97: 155: 21: 112: 63: 41: 123:
woodlands near the base of the Hampton escarpment. The western portion of the plains is in
67: 59:, which extend eastwards from near Eucla for 220 km along the coast of South Australia. 116: 93: 55:, which extend for nearly 200 km along the shore of the bight, and on the east by the 245: 101: 52: 74: 56: 231: 120: 205: 181: 135: 131:
is located in the nature reserve, near the western end of the plains.
210:, Dept. of Earth & Planetary Sciences, Western Australian Museum 88:
The only current human settlements on the Roe Plains are Madura and
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James, NP; Bone, Y; Carter, Bob; Murray-Wallace, CV (June 2006),
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Index


Eucla, Western Australia
plain
Western Australia
Great Australian Bight
Baxter Cliffs
Bunda Cliffs
Hampton Tableland
Nullarbor Plain
Eyre Highway
Madura
Eucla
Mundrabilla
Madura Station
Mundrabilla Station
Twilight Cove
Cocklebiddy
Hampton bioregion
mallee
eucalypt
Nuytsland Nature Reserve
Eyre Bird Observatory
Neogene
"Crossing the Nullarbor"
Origin of the Late Neogene Roe Plains and their calcarenite veneer: implications for sedimentology and tectonics in the Great Australian Bight
A guide to the fossils of the Roe Plains

Roe Plains
Categories
Hampton bioregion

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