...tendency to split along the lines of bedding. An important feature in the joints of stratified rocks is the direction in which they intersect each other....running transversely at a right angle or nearly so. The former set is known as dip-joints, because they run with the dip or inclination of the rocks ; the...

...perpendicular, or approximately so, to the planes of bedding, and descend vertically at not very unequal distances, so that the portions of the rock between...first are called "dip joints" or "end joints" by the quarrymen, since they run with the dip or inclination of the rock, whke the last are called " strike...

...perpendicular, or approximately so, to the planes of bedding, and descend vertically at not very unequal distances, so that the portions of the rock between...first are called "dip joints" or "end joints" by the quarrymeu, since they run with the dip or inclination of the rock, while the last are called " strike...

...portions of the rock between them, when seen from a distance, appear like so many wall-like masses. Au important feature of these joints, as mentioned by...first are called "dip joints" or "end joints" by the quarrymen, since they run with the dip or inclination of the rock, while the last are called " strike...

...like so many wall-like masses. An important feature of these joints, as mentioned by this anthority, is the direction in which they intersect each other....strata are inclined from the horizon, and the other ruuning transversely at a right angle, or nearly so. The first are called "dip joints" or "end joints"...

...dominant trends, one coincident in a general way with the direction in which the strata are inclined to the horizon, and the other running transversely at a right angle or nearly so. The former set is known as dip-jointi, because they run with the dip or inclination of the rocks, the latter...

...character that has nearly or wholly obliterated their tendency to split along the lines of bedding. 525 trends, one coincident, on the whole, with the direction...running transversely at a right angle or nearly so. The former set is known as dip-joints, because they run with the dip or inclination of the rocks ; the...

...appear marked off into so many wall-like masses. "An important feature in the joints of stratified rocks is the direction in which they intersect each other....running transversely at a right angle or nearly so." The frequency of joints in the sedimentary rocks varies much and in some deposits they are very plentiful...

...appear marked off into so many wall-like masses. "An important feature in the joints of stratified rocks is the direction in which they intersect each other....running transversely at a right angle or nearly so." The frequency of joints in the sedimentary rocks varies much and in some deposits they are very plentiful...

...tendency 1 1 split along the lines of bedding. An important feature in the joints of stratified rocks is the direction in which they intersect each other....which the strata are inclined from the horizon, and tbi other running transversely at a right angle or nearly so. The former set is known is dip-joints,...