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8822-4 Howe Range

Sites 8822 1 to 10 - Mallacoota to Cape Howe

This information has been developed from the publications:
    • Sites of Geological and Geomorphological Significance in Central Gippsland (1981) by Neville Rosengren, M.S McRae-Williams and S.M Kraemers.
    • Sites of Geological and Geomorphological Significance in the Gippsland Lakes Catchment (1984) by Neville Rosengren.
    • Sites of Geological and Geomorphological Significance in East Gippsland, Victoria (1981) by Neville Rosengren, M.S McRae-Williams
Geological heritage sites, including sites of geomorphological interest and volcanic heritage sites, are under regular revision by the Geological Society of Australia, especially in the assessment of significance and values. Reference should be made to the most recent reports. See the Earth Science Heritage section of the Geological Society of Australia website for details of geological heritage reports, and a bibliography.


Location:

552446. Nine kilometres east of Mallacoota Inlet.

Image:  East Gippsland Sites of Significance
Eastern shore of Gabo Island and Howe Range.

Abstract:

Granite peak and hillslopes with tors.

Access:

A little used 4-wheel drive track leads from near Bucklands farm east of Mallacoota inlet.

Ownership:

Crown Land (Croajingolong National Park).

Geology:

The rock is a red biotite granite of Late Middle to Early Upper Devonian age and is one of the youngest granitic intrusions in eastern Victoria.

Geomorphology:

Howe Hill is a prominent peak with minor tor development. A spur extending south-eastward defines the easternmost limit of, and forms the catchment for, the Howe Flat/Lake Barracoota wetland.

Significance:

Regional. The dark red granite contrasts with the lighter coloured intrusive bodies of East Gippsland. The range has major importance as the catchment for Lakes Barracoota and Wau Wauka.

Management:

Logging, roadworks, and other land use which may result in serious vegetation disturbance should be prohibited in the Howe Range so the water quality in the adjacent lake systems is preserved.

References:

Rosengren, N. J. 1978. The Physiography of Coastal Dunes, East Gippsland, Victoria. M. A. Thesis (Unpub.), University of Melbourne



8822 1 to 10
Sites 8822-1 to 10
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