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Show Figure :n.- TIIe \.rn tul C:l!ion, lookiu~ \l't'Ht from To-JO' ·W<'np. LAVA. \Ve have no difficulty as we float along, and I am able to observe the wonderful phenomena connected with this .flood of lava. · The canon was dC'ubtless filled to a height of twelve or fifteen hundred feet, perhaps hy more than one flood. This would dam the water back; and in cutting through this great lava bed, a new channel has been formed, sometimes on one side, sometimes on the other. The cooled lava, being of firmer texture than the rocks of which the walls are composed, remains in some places; in others a narrow channel has been cut, ·leaving a line of basalt on either side. It is possible that the lava cooled faster on the sides against the walls, and that the centre ran out; but of this we can only conjecture. There aro other places, where almost the whole of the lava is gone, patches of it only being seen where it has caught on the walls. As we float down, we can see that it ran out into side canons. In some places this basalt.has a fine, columnar structure, often in concentric ptisms, and masses of these concentric columns have coalesced. In some places, when the flow occurred, the canon was probably at about the same depth as it is now, for we can see where the basalt has rolled out on the sands, and, what seems curious to me, the sands are not melted or metamorphosed to any appreciable extent. In places the bed of the river is of sandstone or limestone, in other places of lava, showing that it has all been cut out again where the sandstones and limestones appear; but there is a little yet left where the bed is of lava. What a conflict of water and fire there must have been here l Just imagine a river of molten rock, running down into a river of melted snow. What a seething and boiling of the. waters; what clouds of steam rolled into the heavens l Thirty five miles to day. Hurrah l August ~6.-~.I:'he canon walls are steadily becoming higher as wo advance. They are still bold, and nearly vertical up to the terrace. We still see evidence of the eruption discovered yesterday, but the tl1ickness of t.he basalt is decreasing, as we go down tho stream; yet it has been reinforced at points by streams that have come down from volcanoes standing on the ten-ace above~ but which we cannot see from the river below. Since we left the Colorado Chiquito, we have seen no evidences that the tribe of Indians inhabiting the plateaus on either ~llle ever come down |
