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The glacial beds of Little Peppermint Bay, Tasmania
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Abstract
Little Peppermint Bay is a small arm of the sea on
the western side of D'Entrecasteaux Channel, abont 27
miles south of Hobart. The nearest point at which the
Channel steamers call is Woodbridge, or Peppermint Bay,
about half a mile south of the beds described in this
paper.The prevailing beds in the locality belong to thePermo-
Carboniferous series, and have, over a large area, a fairly
uniform dip to the S.E., at about an angle of 30C. They
are intruded into by two distinct types of igneous rocks,
viz., the Oyster Cove porphyries and the diabase greenstone,
and, near the contacts, are disturbed to a considerable
extent.
Item Type: | Article |
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Authors/Creators: | Hogg, EG |
Keywords: | Royal Society of Tasmania, Van Diemens Land, VDL, Hobart Town, natural sciences, proceedings, records |
Journal or Publication Title: | Papers & Proceedings of the Royal Society of Tasmania |
Collections: | Royal Society Collection Royal Society Collection > Papers & Proceedings of the Royal Society of Tasmania |
Additional Information: | In 1843 the Horticultural and Botanical Society of Van Diemen's Land was founded and became the Royal Society of Van Diemen's Land for Horticulture, Botany, and the Advancement of Science in 1844. In 1855 its name changed to Royal Society of Tasmania for Horticulture, Botany, and the Advancement of Science. In 1911 the name was shortened to Royal Society of Tasmania. |
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