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Books Bücher 1 - 10 von 17 in In the annexed diagram the flat surfaces of rock A, B, C, represent exposed faces...
" In the annexed diagram the flat surfaces of rock A, B, C, represent exposed faces of joints, to which the walls of other joints, JJ, are parallel. SS are the lines of stratification ; DD are lines of slaty cleavage, which intersect the rock at a considerable... "
A MANUAL OF ELEMENTARY GEOLOGY - Seite 469
von SIR CHARLES LYELL, M.A. F.R.S. - 1853
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Elements of geology

sir Charles Lyell (bart.) - 1838
...therefore, must often have resulted from one of the last changes superinduced upon sedimentary deposits.* In the annexed diagram the flat surfaces of rock A,...JJ, are parallel. SS are the lines of stratification ; CC are lines of slaty cleavage, which intersect the rock at a considerable angle to the planes of...
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Elements of Geology

Sir Charles Lyell - 1838 - 543 Seiten
...therefore, must often have resulted from one of the last changes superinduced upon sedimentary deposits.* In the annexed diagram the flat surfaces of rock A,...JJ, are parallel. SS are the lines of stratification ; CC are lines of slaty cleavage, which intersect the rock at a considerable angle to the planes of...
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Elements of Geology

Sir Charles Lyell - 1839 - 316 Seiten
...therefore, must often have resulted from one of the last changes superinduced upon sedimentary deposits.:): In the annexed diagram the flat surfaces of rock A,...are parallel. SS are the lines of stratification; CC are lines of slaty cleavage, which intersect the rock at a considerable angle to the planes of stratification....
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Elements of Geology

Sir Charles Lyell - 1845 - 316 Seiten
...impossible, after carefully studying the appearances, to decide upon the class to which they belong.* In the annexed diagram the flat surfaces of rock A,...JJ, are parallel. SS are the lines of stratification ; CC are lines of slaty cleavage, which intersect the rock at a considerable angle to the planes of...
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Elements of Geology

Sir Charles Lyell - 1846 - 305 Seiten
...therefore, must often have resulted from one of the last changes superinduced upon sedimentary deposits.:): In the annexed diagram the flat surfaces of rock A,...JJ, are parallel. SS are the lines of stratification ; CC are lines of slaty cleavage, which intersect the rock at a considerable angle to the planes of...
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Elements of Geology: Intended for the Use of Students

Samuel St. John - 1851 - 334 Seiten
...planes. In Figure 91, the flat surfaces, ABC, represent Fig. 91. Stratification, Joints, and Cleavage. exposed faces of joints, to which the walls of other joints, JJ, are parallel : ss, are lines of stratification ; Ce, are lines of slaty cleavage intersecting the planes of stratification...
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Elements of Geology: Intended for the Use of Students

Samuel St. John - 1851 - 334 Seiten
...cleavage planes. In Figure 91, the flat surfaces, ABC, represent Stratification, Joints, and Cleavage. exposed faces of joints, to which the walls of other joints, JJ, are parallel: ss, are lines of stratification; CC, are lines of slaty cleavage intersecting the planes of stratification...
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Elements of geology, intended for the use of students

Samuel St. John - 1852 - 334 Seiten
...planes. In Figure 91, the flat surfaces, ABC, represent Fig. 91. Stratification, Joints, and Cleavage. exposed faces of joints, to which the walls of other joints, JJ, are parallel: ss, are lines of stratification; cc, are lines of slaty cleavage intersecting the planes of stratification...
Vollansicht - Über dieses Buch

Elements of Geology: Intended for the Use of Students

Samuel St. John - 1854 - 334 Seiten
...cleavage planes. In Figure 91, the flat surfaces, ABC, represent Stratification, Joints, and Cleavage. exposed faces of joints, to which the walls of other joints, jj, are parallel: s s, are lines of stratification; cc, are lines of slaty cleavage intersecting the planes of stratification...
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ELEMENTS OF GEOLOGY, INTENDED FOR THE USE OF STUDENTS.

SAMUEL ST. JOHN - 1854
...cleavage planes. In Figure 91, the flat surfaces, ABO, represent Stratification, Joints, and Cleavage. exposed faces of joints, to which the walls of other joints, jJ, are parallel : Ss, are lines of stratification ; CC, are lines of slaty cleavage intersecting the planes of stratification...
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