Document Pages

34 Pages
Page 18
{ "text": "Sandset\nWaldsum\nsofter cl.\ngndbld, et,\nprv\nchert\nNot bldl.\nchert\nExcellent bldl\nTop layer (leg.\nTotal\n\n1\n4-5\n6\n9 3/8 15°\n\n\n\nBride Ed D\n\n\nCrude\n\n\nSandmng\n\n\n\n\n\n20 1/2\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n [TRANSCRIPTION_TRUNCATED_DUE_TO_LOOP]
Page 21
New Point Clinton to 25 feet below New Point RR. 968 New Point J M, Clay, 5 ft - 10 ft, 1-3 feet of rip rap, clint, 3 in. well tins, light rubble. 12 in. 4/3 curbing. 8 in footing, walk slate, gutter flag, crossing, clint modules near middle. 8 in, like above but better also with clint 8 in. like above 15 m 9/6 roughly scarred limestone all in the middle, a little white clay, 7 in footing. 6 in very fine dressed work, window sills + 8 in - 10 in. footings, dressed work, 4 m flagging, curbing, ashlar, 4 in light free clay, rubble, 10 in regular flint, footings, 2 1/2 in thick scrap, sidewalks, 9 in good stone all layers dressed 6/3 work street to building 3m coping. shed walk, cur. 16 in 9/7 first block, bridge work heavy coping, ateley curbing dry sides rain table. works streched longitudially. planning a cent of argillaceous bedding. 20 in scrap stone, clay, clint, 12 in often with 4 m. 9 scraping on top and lower &d anyga for rip rap, foundations. 24 in bridge work, clay + limestone concrete mixed. Exposed, used 8 years for bridgework, used for backing. 12 in footings percent for anything else bridge work 40 in 15/24 bagrod, clay + limestone surface sometimes lown 10 inches so far themselves form a quite good ledge, tar for footings + bridge coping, 668 in about 5 in. 9 good at me after scale is taken off the top and red at me is 1/2 when by the top inm used for rubble footings curbing clint m. both in. sometimes hangs together and is 9 1/2 in. thick, used for footings curb culvert - corking where blocks but little flint there hanging together, a. About 1 mile south of St. Marys, Sollman bnm Clinton at least 4 feet thick 17 feet below RR at New Point. Exposed bed exposed w hand a short distance Eastward.
Page 29
{ "text": "\"The Carboniferous period, though in its\nchief subdivisions post-Cretaceous and the Caledonian, extends to an immense depth and range of area.\nThese seas were connected with the ocean in the south,\nand with it in the north.\nThe latter was very large in area. That great rise to land depression\nwas formed in this vast depression\nwhich had divided into two great fields,\nthe Carboniferous post-Cretaceous, and the Caledonian.\nIn each of these the sea's advancing\nfronts were marked by a series of\nshelves (Cathrein-les co. 2000)\nand the eastern border of Britain\nseparated these two seas; Eastern\nScotland, Ireland and northern\nEngland forming the land which fell in the western border and\nthe southern border of Scotland.\nThe Devonian or Tertiary land\nlastly divided into a series of states\nby the Irish Sea lying in a north-\nsouth direction across the state,\nand extending in place in the\nnorth, Caledonian and Silurian\na high ridge at Scotland.\nA long narrow belt of land\nand the eastern border of England\nand the Devonian border of Britain\nfalling in the western border and\nthe southern border of Scotland.\nThe Devonian or Tertiary land\nlastly divided into a series of states\nby the Irish Sea lying in a north-\nsouth direction across the state,\nand extending in place in the\nnorth, Caledonian and Silurian\na high ridge at Scotland.\nA long narrow belt of land\nand the eastern border of England\nand the Devonian border of Britain\nfalling in the western border and\nthe southern border of Scotland.\nThe Devonian or Tertiary land\nlastly divided into a series of states\nby the Irish Sea lying in a north-\nsouth direction across the state,\nand extending in place in the\nnorth, Caledonian and Silurian\na high ridge at Scotland.\nA long narrow belt of land\nand the eastern border of England\nand the Devonian border of Britain\nfalling in the western border and\nthe southern border of Scotland.\nThe Devonian or Tertiary land\nlastly divided into a series of states\nby the Irish Sea lying in a north-\nsouth direction across the state,\nand extending in place in the\nnorth, Caledonian and Silurian\na high ridge at Scotland.\nA long narrow belt of land\nand the eastern border of England\nand the Devonian border of Britain\nfalling in the western border and\nthe southern border of Scotland.\nThe Devonian or Tertiary land\nlastly divided into a series of states\nby the Irish Sea lying in a north-\nsouth direction across the state,\nand extending in place in the\nnorth, Caledonian and Silurian\na high ridge at Scotland.\nA long narrow belt of land\nand the eastern border of England\nand the Devonian border of Britain\nfalling in the western border and\nthe southern border of Scotland.\nThe Devonian or Tertiary land\nlastly divided into a series of states\nby the Irish Sea lying in a north-\nsouth direction across the state,\nand extending in place in the\nnorth, Caledonian and Silurian\na high ridge at Scotland.\nA long narrow belt of land\nand the eastern border of England\nand the Devonian border of Britain\nfalling in the western border and\nthe southern border of Scotland.\nThe Devonian or Tertiary land\nlastly divided into a series of states\nby the Irish Sea lying in a north-\nsouth direction across the state,\nand extending in place in the\nnorth, Caledonian and Silurian\na high ridge at Scotland.\nA long narrow belt of land\nand the eastern border of England\nand the Devonian border of Britain\nfalling in the western border and\nthe southern border of Scotland.\nThe Devonian or Tertiary land\nlastly divided into a series of states\nby the Irish Sea lying in a north-\nsouth direction across the state,\nand extending in place in the\nnorth, Caledonian and Silurian\na high ridge at Scotland.\nA long narrow belt of land\nand the eastern border of England\nand the Devonian border of Britain\nfalling in the western border and\nthe southern border of Scotland.\nThe Devonian or Tertiary land\nlastly divided into [TRANSCRIPTION_TRUNCATED_DUE_TO_LOOP]