These deposits are hosted in palaeochannels filled with Cainozoic sediments and sourced their uranium from uranium-rich Palaeo-to Mesoproterozoic rocks of the Mount Painter Inlier and the Olary Domain of the Curnamona Province.
32.
Further to the north still, sandwiched between these intake fields and the steep slopes of the Pennine escarpment itself lies a complex geological zone known as the Cross Fell Inlier ( see Burgess and Wadge ).
33.
In one data set, a value of 1.1 may already be an outlier, in another dataset and parameterization ( with strong local fluctuations ) a value of 2 could still be an inlier.
34.
But similar rock also occurs in the Rimrock Lake Inlier, about 75 km south of the OWL and just west of the projected trace of the SCF, and also in the Klamath Mountains of southwestern Oregon.
35.
The whole North Pennines AONB, of which the Inlier forms part, is in fact of such interest to geologists that in 2003 it was designated a Geopark under a Unesco programme to promote public interest in geology.
36.
Other similar rock has been found at the Rimrock Lake Inlier ( bottom of diagram ), in the San Juan Islands, and in the Pacific Coast Complex along the West Coast Fault on the west side of Vancouver Island.
37.
The central portion of this zone, between Usk and Pontypool, comprises the outcrop of the older shales, limestones and sandstones and, surrounded as it is by outcrops of younger rocks, is traditionally referred to as the Usk Inlier.
38.
The Greensand inlier is a dome shaped area of hard, coarse, olive-green coloured sandstone rock which has had its covering of softer chalk eroded away by 60 million years of weathering since the region was lifted out of the sea.
39.
The resulting algorithm is dubbed Guided-MLESAC . Along similar lines, Chum proposed to guide the sampling procedure if some a priori information regarding the input data is known, i . e . whether a datum is likely to be an inlier or an outlier.
40.
The oldest rocks found on the Watermillock Common ridge occur on the lower south eastern slopes ( above Ullswater ) where faulting has brought to the present surface an inlier of mudstone from the "'Tarn Moor Formation "', the latest part of the Skiddaw Group.
