This information has been developed from the publications:
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Location: | 9-213310. Two kilometres south of Gellibrand and 100 m north east of Site 9.5. | |
Access: | Gellibrand-Beech Forest Road. | |
Ownership: | Private land. | |
Geology: | Gravel beds contained in the Dilwyn Formation include large pebbles of material that has not been derived from the Otway Group. Kenny (1938) suggested that some may have originated in the Grampians area but no further study of origin or mode of transport has been made since his work. | |
Significance: | Regional. The coarseness of the gravel beds is unusual in the Tertiary sediments of the Gellibrand area. |