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Transactions of the Geological Society of Glasgow
  • Language: en
  • Pages: 348

Transactions of the Geological Society of Glasgow

  • Type: Book
  • -
  • Published: 1867
  • -
  • Publisher: Unknown

None

Transactions
  • Language: en
  • Pages: 352

Transactions

  • Type: Book
  • -
  • Published: 1879
  • -
  • Publisher: Unknown

None

Transactions of the Geological Society of Glasgow
  • Language: en
  • Pages: 418

Transactions of the Geological Society of Glasgow

  • Type: Book
  • -
  • Published: 1868
  • -
  • Publisher: Unknown

None

Transactions of the Geological Society of Glasgow
  • Language: en
  • Pages: 354

Transactions of the Geological Society of Glasgow

  • Type: Book
  • -
  • Published: 1867
  • -
  • Publisher: Unknown

None

Transactions of the Glasgow Geological Society, Being a Paper on the Geology of the Campsie District
  • Language: en
  • Pages: 45
Transactions
  • Language: en
  • Pages: 132

Transactions

  • Type: Book
  • -
  • Published: 1963
  • -
  • Publisher: Unknown

None

Transactions of the Geological Society of Glasgow
  • Language: en

Transactions of the Geological Society of Glasgow

  • Type: Book
  • -
  • Published: 1910
  • -
  • Publisher: Unknown

None

History of the Geological Society of Glasgow, 1858-1908
  • Language: en
  • Pages: 376

History of the Geological Society of Glasgow, 1858-1908

  • Type: Book
  • -
  • Published: 1908
  • -
  • Publisher: Unknown

None

Transactions of the Geological Society of Glasgow 1937-44
  • Language: en

Transactions of the Geological Society of Glasgow 1937-44

  • Type: Book
  • -
  • Published: 1945
  • -
  • Publisher: Unknown

None

Transactions of the Geological Society of Glasgow
  • Language: en
  • Pages: 248

Transactions of the Geological Society of Glasgow

Excerpt from Transactions of the Geological Society of Glasgow: Session 1865-66 The three great divisions into which the superficial deposits of the district in and around Glasgow naturally group themselves, the period of land ice, represented by the boulder clay; the period of sea deposits, represented by the boreal shell beds; and the recent or human period, represented by the sand and gravel beds, containing canoes - certainly in part, if not wholly, of fresh water origin - are not only better exhibited in this district than anywhere else, but the amount of observation bestowed upon them has rendered this classic region the most typical among the post tertiary deposits of Scotland. About ...