AIM: To provide pre-detail coverage over the faulted Camelback High feature observed on 2 dynamite lines recorded by Esso in 1969, and as a basement anomaly on the 1:100 000 regional gravity map. The closest well was Lucindale 1, 11 km to the east in PEL 27. The lines were continued to the SW to encompass the Lake Eliza High, a tying-in with wells Lake Eliza 1 and 2, to identify possible structuring in a region of previously limited seismic coverage. A regional line was extended to the Lake George 1 well near Beachport to give a further seismic reference point. The lines were spaced a nominal 2 km apart with 3 NW-SW strike lines. The data were intended to be recorded with sufficient resolution, both spacially and in frequency content, to observe possible structure within the Pretty Hill Sandstone and Eumeralla Formation. RESULTS: Multifold lines recorded by Australian Aquitaine in Rendelsham and OTSA-81 Seismic Surveys, intersecting Konetta South Seismic Survey lines were reprocessed. Follow up work is recommended over 4 leads and the Camelback feature. Energy source: Vibroseis. CDP coverage: 2000%. Recording mode: Digital / DFSV/FT-1. 296 km line of 120 channels. SP/VP interval: 75 metres. Survey dates: 25/2/85 - 6/4/85.