This information has been developed from the publications:
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Location: | 7 - 000239. Gellibrand River valley two kilometres north west-west of Mt. McKenzie. (This site overlaps Site 7.9.) |
Access: | Off Gellibrand River Road. |
Ownership: | Private land and some Crown Land. |
Geomorphology: | This site is distinctive for the high levee banks that occur in a narrow valley sector. |
The levees indicate a change from a predominantly erosive river regime to an aggradational phase when floodplain sediments including levee banks were deposited. It is probable that levee growth is now very limited as the river is deeply incised into floodplain deposits. | |
Significance: | Regional. The Gellibrand River has levee banks at several localities and this is one of the best inland examples. |
7.9 to 7.10 |