Bulletin, Issue 23State of Ohio, Department of Natural Resources, Division of Geological Survey., 1921 - Geology - 190 pages |
From inside the book
Results 1-5 of 76
Page 11
... foot of gage , exposing characteristic , gently sloping gravel bottom of channel ... A. - View up - stream at Riffle 13 , with bars and snags . B. - View up - stream above Riffle 15 ; bank on right was so far cut back by the 1913 flood ...
... foot of gage , exposing characteristic , gently sloping gravel bottom of channel ... A. - View up - stream at Riffle 13 , with bars and snags . B. - View up - stream above Riffle 15 ; bank on right was so far cut back by the 1913 flood ...
Page 13
... foot , sloping from them to the distant left are remnants of the Illinoian gravel terrace . B. - View eastward from the northeast corner Section 21 , Springfield Township , across the maturely dissected Illinoian gravel terrace , to the ...
... foot , sloping from them to the distant left are remnants of the Illinoian gravel terrace . B. - View eastward from the northeast corner Section 21 , Springfield Township , across the maturely dissected Illinoian gravel terrace , to the ...
Page 16
... foot of soil . This material could not be excavated with the light tools furnished or even with proper equipment in the time available . As a consequence there was a large and needless loss of life . " In part of the Lorraine sector the ...
... foot of soil . This material could not be excavated with the light tools furnished or even with proper equipment in the time available . As a consequence there was a large and needless loss of life . " In part of the Lorraine sector the ...
Page 19
... foot contour would pass through all points 700 feet above sea level , and would be found on Foth sides of any valley whose bottom is less than 700 feet and whose bounding hills are more than 700 feet above sea level , winding around the ...
... foot contour would pass through all points 700 feet above sea level , and would be found on Foth sides of any valley whose bottom is less than 700 feet and whose bounding hills are more than 700 feet above sea level , winding around the ...
Page 24
... foot of the next escarpment to the westward . The escarpments in Ohio compare favorably in height and dissection with the French occurrences but the back slopes in Ohio are much gentler than the corresponding French features . Causes ...
... foot of the next escarpment to the westward . The escarpments in Ohio compare favorably in height and dissection with the French occurrences but the back slopes in Ohio are much gentler than the corresponding French features . Causes ...
Other editions - View all
Common terms and phrases
30 feet A.-View Allegheny Plateau altitude bank bed rock Berea Grit bottom bowlder clay Camp Sherman quadrangle channel Chillicothe Colerain Township concrete County Line bridge cuesta Cuyahoga Deer Creek deposits depth dissected drift Dry Run eastern eastward escarpment excavations feet deep feet thick flat flood plain flow foot forested Fork of Paint formation geology glacial gravel terraces Green Township ground water hilltops Hopetown ice sheet Illinoian gravels inches Indian Creek kame Kinnikinnick knee deep lower slopes Lowland margin miles Mount Logan narrow North Fork northeast northward numerous Ohio shale outcrops Paint Creek Paint Creek Valley pebbles peneplain Pike places Plate Poplar Ridge portion probably Ralston Run Ridge riffles rise road rock hills Rocky Knob rolling sand sandstone Scioto River Scioto Valley shallow side snags southward southwest Springfield Township springs stage steep streams subdivision Sugar Loaf surface topography trenches upper Walnut Creek weathering westward