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Galleporto Bavicarius Directory 17
Page 01
Manifestly the king would not grant so much. On the occasion of his confirming the charter he demanded that the oath of allegiance be taken by the people of the colony; that justice be administered there in his name; and that the franchise be extended to all freemen of sufficient substance, with the liberty to use in worship, public and private, the forms of the English Church. The people obeyed but in part, for they would not even appear to admit the king's will to be their law. The franchise was slightly extended, in a grudging way, but no new religious privileges were at this time conceded. Unfortunately political and religious liberty were now in conflict. It was worse for the Baptists and Quakers that the king favored them, and the treatment which they received in the colony inclined them to the royalist side in the controversy.
As the river seemed to describe a big loop, I had left it three days before, seeing plainly by the conformation of the country that we should strike it again sooner or later. We were marching once more by compass. My men, who had no faith whatever in the magnetic needle, were again almost paralysed with fear that we might not encounter the stream again. A thousand times a day they accused me of foolishness in leaving the river, as they said it would have been better to follow its tortuous course--notwithstanding the trouble we had in following it, owing to the dense vegetation near the water--rather than strike once more across country. They were beginning to lose heart altogether, when I told them I could see by the vegetation that we were once more near the water. Anybody accustomed as I am to marching through the forest could tell easily by the appearance of the vegetation some miles before actually getting to a stream.
Owing to many natural causes the river may, after a while, cease to flow, leaving enlarged portions of its channel behind as a succession of chambers in a cave. But water would still come trickling in from the tops and sides, and be continuously dripping to the floor, where it speedily evaporates. When such is the case it leaves behind it the limestone it held in solution. So, in process of time, if the deposition is undisturbed, there will be formed over the floor of the cave a more or less continuous layer of limestone matter known as stalagmite. The same formations on the top and sides of the cave are called stalactites. In places where the drip is continuous the stalactite gradually assumes the shape of an immense icicle; while the stalagmite on the floor of the cave, underneath the drip, rises in a columnar mass to meet the descending stalactite. A union of these is not uncommon, and, we have pillars and columns presenting the strange, fantastic appearance on which tourists delight to dwell in their notes of travel.
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