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8622-2 Dock Inlet

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:

620166. 11 kilometres west of Bemm township.

Image:  East Gippsland Sites of Significance
Dock Inlet. River delta (A). Spit (A).

Abstract:

Freshwater coastal lagoon.

Access:

Unformed track from Bemm River or Cape Conran.

Ownership:

Crown Land.

Geology:

Quaternary dune sands and swamp deposits.

Geomorphology:

Dock Inlet is a freshwater lagoon fed by a small stream system that drains heath and woodland south of the old Coast Road. The lagoon occupies a former embayment which has been enclosed by accumulation of barrier and dune sands and is completely isolated from the sea. The former sea cliff that is now a bluff marking the inner edge of Dock Inlet is cut in consolidated Pleistocene sands which is exposed along the channel of the main inflowing stream. This sinuous channel is in places only two metres wide but is three to four metres deep. Even though the catchment area is small, the holding capacity must be high due to the sandy substrate and the dense cover of swampy heath and stream flow is permanently maintained. The lake water is fresh with salinity below 5 parts per thousand. Shorelines are fringed by
Eleocharis sphacelata and Triglochin procera. The lake averages two metres depth but deepens to 3.5 metres on the western side. It is gradually shallowing by encroachment of the fringing swamp vegetation and by addition of dune sands that are blown over the coastal barrier. At low water level the lake is separated into two basins by a sand bar and spit extending from the southern shoreline.

The main body of Dock Inlet had no overflow channel to the sea although an area of swamp and low dunes that extend to the west probably mark the site of a former tidal inlet. A small reed and sedge-filled former lagoon one kilometre east of Dock Inlet represents a further stage in the swamp reclamation of a similar fresh water system.


Significance:

State. Dock Inlet is a classic example of a fresh water lagoon separated from the sea by only a low sand barrier but rarely subject to wave washover. Of particular interest are the deep river channel that feed the lake, the exposures of older dune materials in the shoreline bluff and the varied shoreline morphology.

Management:

Because it is completely enclosed Dock Inlet can be rapidly degraded by over-intensive use – particularly power boating, and this should be prohibited. The catchment area, being small, should be protected in full from logging or land clearing. Development of visitor or camping facilities would be incompatible with maintaining the pollution free lake environment which is necessary to retain the aquatic vegetation.

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