Report On the Geology of the South West Part of Nelson And the Northern Part of
Report On the Geology of the South West Part of Nelson And the Northern Part of
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In the Upper Buller Valley the only evidence of . South-West Nelson and Northern Westland. 47 glacier action is the moraine stretched across the Manila, seven miles below Walker's Home Station. This is unmistakable in its character the general character of the material, the hummocky outline of the surface, and the large far-transported blocks of rock, still perfectly angular, amply testify to the fact.
(b. ) River Deposits formed prior to the Advance of the Glaciers. At Ross the deposits in the... flat are partly reconstructed glacier material, and partly river-gravels that were deposited prior to the advance of the glaciers. The various alternations of these beds are well seen in the workings of the Ross United Company's Claim, and there can be no doubt that the greater area of the Ross Flat towards the sea contains the like deposits.
In the country between the Totara and Rimu it is uncertain if any of the gravels seen along the road-line do underlie the glacier deposits, but along Back Creek, and in the face of the terrace overlooking the low grounds of the Hokitika, it is abundantly demonstrated that river gravels underlie the glacier deposits.
What to read after Report On the Geology of the South West Part of Nelson And the Northern Part of?
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To quickly assess the difficulty of the text, read a short excerpt:
In the Upper Buller Valley the only evidence of . South-West Nelson and Northern Westland. 47 glacier action is the moraine stretched across the Manila, seven miles below Walker's Home Station. This is unmistakable in its character the general character of the material, the hummocky outline of the surface, and the large far-transported blocks of rock, still perfectly angular, amply testify to the fact.
(b. ) River Deposits formed prior to the Advance of the Glaciers. At Ross the deposits in the... flat are partly reconstructed glacier material, and partly river-gravels that were deposited prior to the advance of the glaciers. The various alternations of these beds are well seen in the workings of the Ross United Company's Claim, and there can be no doubt that the greater area of the Ross Flat towards the sea contains the like deposits.
In the country between the Totara and Rimu it is uncertain if any of the gravels seen along the road-line do underlie the glacier deposits, but along Back Creek, and in the face of the terrace overlooking the low grounds of the Hokitika, it is abundantly demonstrated that river gravels underlie the glacier deposits.
What to read after Report On the Geology of the South West Part of Nelson And the Northern Part of?
You can find similar books in the "Read Also" column, or choose other free books by Alexander Mackay to read onlineMoreLess
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