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The strata dipped to the Northwest with an average dip angle of 10 degrees.
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Strata dip at ∼1.75% SSE and include a prominent SSE-NNW structural fabric dominated by a ridge that corresponds to a Precambrian basement fault and overlying flexure.
The rock strata here dip 10°-15° 10°-15°souto-westhe
The strata of mining area are generally monocline strata dipping into west with a dip angle of about 1 3°, where faults are rare and structure is simple.
The interior part of the basin is characterized by horizontal or gently dipping strata (<3°), especially for the Mesozoic and Cenozoic strata, whereas the strata along the margins have been subjected to significant folding and faulting since the Late Triassic.
During the regressive periods, dipping strata were developed, while erosional surfaces and incised valleys were formed during the lowstands of sea level.
However, first- and second-order basins situated on the flanks of moderately dipping strata are strongly elongated with circularity ratios between 0.4 and 0.5 (Chow 1964).
Shallow highly weathered and fractured strata overlie unweathered, gently dipping, fractured strata that become progressively less fractured with depth.
Below the weathered and highly fractured strata, and to depths of at least 50 meters (m), groundwater flow and contaminant transport is primarily in bedding-plane-oriented fractures in thin fissile high-carbon strata, and in fractured, laminated strata of the gently dipping mudstones.
At the margins of the Kimberleys (in the Fitzroy region and in the Durack Range) and in the southern part of the Pilbara, in the Ophthalmia Range, dipping rock strata have been differentially eroded to form ridges and valleys.
The strata are densely jointed, dipping at 35° 38° towards the valley.
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