Manual of Geology, Treating of the Principles of the Science: With Special ...

Cover Manual of Geology, Treating of the Principles of the Science: With Special ...
Manual of Geology, Treating of the Principles of the Science: With Special ...
James Dwight Dana
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In Fig. 235 the cone to the left shows the dip of the layers of tufe inward toward the center of the crater and outward, down the outer slopes. Driblets pile up the fantastic driblet-cone, which has no crater but simply a hole for the projection of lava in small liquid masses, drops, drib- lets, or worm-like streamlets.
284.
235.
Tnfa-cones, 0«ha. Fig. 234, a, the tafa-cone, Diamond Head, eaat of Honolalu, the exterior eroded ; h, e, other amaller eonee; Fig. 286, Koko Head tufa-cones, east cap
...e of Oahn, the one to the left cat through by the sea, that to the right eroded inaide aa well aa outaide. D.
Still another kind of cone, occasionally observed in Kilauea, is the debris- oone, made at times in Halemaumau after a discharge out of the masses or fragments that fall into the basin from its steep sides. (See Fig. 231.) Drlblet^wne of Kilauea. D. '40.
Driblet-cone. Brigbara, '64.
At an eruption, the discharged lava : (1) may flow down the mountain in great streams from the crater at the summit ; or (2) may escape to the surface through breaks or fissures made by the eruptive forces in the moun- tain's sides, and thence spread away in streams ; or (3) it may flow off through fissures into underground cavities between the old lava streams of the mountain, or it may only fill the opened fissures.


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