CĂRȚI ÎN ENGLEZĂ ÎN LEGĂTURĂ CU «FALSE BEDDING»
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Ten years later E. T. Cox, then State Geologist, gave a brief description of these
localities, but ascribed the inclined beds to false bedding.:}: Oblique or false
bedding on a large scale is an unusual phenomenon in limestones. The seas in ...
Indiana. Dept. of Geology and Natural Resources, 1904
Ten years later E. T. Cox, then State Geologist, gave a brief description of these
localities, but ascribed the inclined beds to false bedding.:}: Oblique or false
bedding on a large scale is an unusual phenomenon in limestones. The seas in ...
Indiana. Dept. of Geology and Natural Resources, 1904
3
Manual of Geology: Theoretical and Practical
FALSE BEDDING. 73 False Bedding. — But the coarser flagstones of the same
coal districts are often composed of laminae, laid at various angles to the plane of
the bed, and in consequence producing a rough, uneven, shattery surface, and ...
John Phillips, Robert Etheridge, Harry Govier Seeley, 1885
Ten years later E. T. Cox, then State Geologist, gave a brief description of these
localities, but ascribed the inclined beds to false bedding. ^ Oblique or false
bedding on a large scale is an unusual phenomenon in limestones. The seas in
which ...
The true bedding of the rock is very faint, scarcely discernible in some places, but
the false bedding is in most places rather pronounced, shown generally by a
banding along the false bedding planes, and in some places a cleavage or
parting ...
Pennsylvania State University, 1897
6
Annual Report of the Pennsylvania State College for the Year ...
The true bedding of the rock is very faint, scarcely discernible in some places, but
the false bedding is in most places rather pronounced, shown generally by a
banding along the false bedding planes, and in some places a cleavage or
parting ...
7
The Building Materials of Pennsylvania: I.--Brownstones
The true bedding of the rock is very faint, scarcely discernible in some places, but
the false bedding is in most places 'rather pronounced, shown generally by a
banding along the false bedding planes, and in some places a cleavage or
parting ...
Thomas Cramer Hopkins, 1896
The true bedding of the rock is very faint, scarcely discernible in some places, but
the false bedding is in most places rather pronounced, shown generally by a
banding along the false bedding planes, and in some places a cleavage or
parting ...
Pennsylvania State College, 1897
9
Journal and Proceedings of the Royal Society of New South Wales
There are two kinds of strati lication, namely, large divisional lines from one foot
to six feet and more apart, and cross stratification or false bedding. Two
peculiarities of this formation will now be mentioned : — 1. The curious dip of the
beds. 2.
10
Official Documents, Comprising the Department and Other ...
The true bedding of the rock is very faint, scarcely discernible in some places, but
the false bedding is in most places rather pronounced, shown generally by a
banding along the false bedding planes, and in some places a cleavage or
parting ...
