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Download Complete Bulletin (7.2 MB)
Publication Date
4-1999
Series Number
4359
Abstract
Almost all the soils of the Swan coastal plain are formed by material deposited by sea, rivers and wind. The Yilgarn Block, east and south of the Scarp bordering the Swan Coastal Plain (Fig. 1), rose about 40 to 50 million years ago. This caused erosion of the block by rivers and streams, and the eroded material was either deposited onto the Swan Coastal Plain or washed into the sea. The eroded material formed new soils on the Plain.
Broadly there are two major types of soils on the Coastal Plain. The first is a series of dune system near the coast formed as a result of deposits from the sea, and including material originally derived from erosion of the Yilgarn block mixed with material from the sea. Once formed, the dunes can be eroded by strong winds. The sand is mostly eroded from the dunes nearest the coast, and is re-deposited on the dunes further inland. The second major soil types are a series of soils formed by deposits directly eroded from the Yilgarn block and which comprise soils of the Pinjarra plain, occurring between the dunes and the scarp. There is a third, very narrow strip of soil, called the ridge hill shelf, next to the scarp, formed from material eroded from the scarp. It is too small to be of any significance.
Number of Pages
13
ISSN
1326 — 415X
Publisher
Agriculture Western Australia
City
Perth
Keywords
Soils, Soil management, Swan Coastal Plain, Dune system, Western Australia
Disciplines
Agricultural Science | Agriculture | Agronomy and Crop Sciences | Environmental Monitoring | Hydrology | Natural Resources and Conservation | Natural Resources Management and Policy | Sedimentology | Soil Science
Recommended Citation
Bolland, M.
(1999), Bulletin 4359 - Soils of the Swan Coastal Plain. Agriculture Western Australia, Perth. Bulletin 4359.
https://library.dpird.wa.gov.au/bulletins/345
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