Annual report of the Board of agriculture of the State of OhioBoard of agriculture, 1867 |
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Pagina 15
... sandstones and bluish argillaceous shales . These strata have offered little resistance to the powerful denuding action to which the whole surface of the northern part of Ohio has been subjected ; as a consequence , they have been ...
... sandstones and bluish argillaceous shales . These strata have offered little resistance to the powerful denuding action to which the whole surface of the northern part of Ohio has been subjected ; as a consequence , they have been ...
Pagina 16
... sandstone , clay and coal , possesses great fer- tility even to the hill - tops . GEOLOG Y. NORTHERN DIVISION - ASHTABULA TO NILES . The geology of the country along the line of the Railroad from the lake shore , forty miles southward ...
... sandstone , clay and coal , possesses great fer- tility even to the hill - tops . GEOLOG Y. NORTHERN DIVISION - ASHTABULA TO NILES . The geology of the country along the line of the Railroad from the lake shore , forty miles southward ...
Pagina 17
... sandstone . This sandstone will sometimes furnish a good grindstone grit , but generally the layers are too thin to make good building stone , and contain protoxide of iron , which , becoming peroxidized by exposure , injures both its ...
... sandstone . This sandstone will sometimes furnish a good grindstone grit , but generally the layers are too thin to make good building stone , and contain protoxide of iron , which , becoming peroxidized by exposure , injures both its ...
Pagina 20
... SANDSTONE NUMBER ONE . Upon the shale last described rests a yellowish sandstone , which , along the line of the railroad in Wethersfield , Austintown , 20.
... SANDSTONE NUMBER ONE . Upon the shale last described rests a yellowish sandstone , which , along the line of the railroad in Wethersfield , Austintown , 20.
Pagina 21
... sandstone last mentioned , with an intervening stratum of blue shale of variable thickness , but probably not over from ten to fifteen feet , lies a collocation of minerals which , from their proximity and individual value , demand ...
... sandstone last mentioned , with an intervening stratum of blue shale of variable thickness , but probably not over from ten to fifteen feet , lies a collocation of minerals which , from their proximity and individual value , demand ...
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