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6.1.4 Volcanic Western Plains with well developed drainage

Transitional to geomorphic unit 6.1.3 are the plains with well developed drainage, which represent the earlier Pliocene volcanic landscapes. Examples of this landform can be seen in the region north-west of Cressy and south-east of Wallinduc, in the area where drainage is well established and ephemeral wetlands are relatively few. These areas are characterised by very planar landscapes with thicker soil development. Towards the Western Uplands to the north, the basalt plains are covered by a thin veneer of sandy and silty outwash deposits.

Associated soil types are predominantly black and brown sodic mottled texture contrast soils.

Geomorphic unit 6.1.4
Soil-landform units

Soil-landform unit
Original unit ID
Unit description
Area (km2)
85
Gently undulating plains (Werneth)
144
39
Low hills (Emu Hill)
3
77
Undulating low hills (south-east of Carranballac)
<0.5
164
Undulating low hills (Cobrico)
16
30
Undulating rise (west of Pitfield)
3
150
Gently undulating basalt rises (Moriac)
150
227
Undulating rises (Moriac)
4
228
Undulating rises (north-west of Mount Duneed)
11
29
Gently undulating plains (Bradvale)
584
112
Undulating plains (Naroghid)
48
224
Gently undulating plains (east of Inverleigh)
11
230
Gently undulating plains (Lara)
3
78
Undulating plains (west of Shelford)
158
154
Level plains (Lake Mudeduke)
6
223
Near level plains (Bannockburn)
17
75
Granitic colluvial slopes (Lismore)
31
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