But when the secondary fissures occurred, the intrusive matter was not only a bastard granite, but with it came also tin and copper. And these metallic lines, which run on Dartmoor from E. to W., and in Cornwall from E.N.E. to W.S.W., are called _lodes_. The cross-cracks do not contain metal. They are called _cross-courses_. In addition there are some capricious veins that do not run in the normal direction, and these are called _counter-lodes_. Their usual direction is N.E. The cross-courses, although without metal, are of considerable value to the miner, because, as he knows well, the best lodes are those which are thus traversed. There is, however, one description of cross-course that is called _floocan_, and which is packed with clay, and holds back water. These are accordingly not cut through if it can possibly be avoided. A very curious feature in the lodes is, that after going down to a variable depth the tin is replaced by copper. Percy was the first to establish this, towards the close of last century. He pointed out that many an old tin mine was in his time worked for copper. And it came to be supposed that this would be found to be an unchanging law: Go deep enough after tin, and you come to copper. But this opinion was shaken when it was found that Dolcoath, the profoundest mine in Cornwall, which had for some time been worked for copper, became next rich in tin. What seems to have been the case was this: when a vent offered, there was a scramble between the two minerals which should get through first and out of the confinement under earth's crust, and now a little tin got ahead; then came copper trampling on its heels, but was itself tripped up by more tin. Now, when the granite came to the surface, it did not have everything its own way, and hold its nose on high, and lord it over every other rock as being the most ancient of all, though not the earliest to put in an appearance. There was a considerable amount of water about. There is plenty and to spare in the west of England now, but we may feel grateful that we do not exist in such detestable weather, nor exposed to such sousing rains, nor have to stand against such deluges, as those which granite had to encounter. Hot, over-hot, it may have been below, but it was cold and horribly wet above. The rains descended; the floods came, and beat on the granite, which, being perhaps at the time warm and soft, and being always very absorbent, began to dissolve. As it dissolved, the water swept away all its component parts, and deposited the heaviest near at hand, and took the lightest far away. Now the heaviest of all were the ore from the veins or lodes, and the water swept this down into the valleys and left it there, but it carried off the dissolved feldspar and deposited it where it conveniently could and when it was tired of carrying it. The former is stream-tin; the latter is china clay.