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Excellent paved approach roads Ur son is a hoe shirt .make Petrified Forest National Monument easily accessible by car, tshirtclassic and it can be visited throughout the year. US 66, crossing the area near the Painted Desert, is the approach from the east. Travelers from the southeast, south, and west enter from US 260. The monument road connects these two main highways and leads through the more interesting parts of the area. This road through the monument is closed to through travel at night. Travelers by rail must obtain privately operated cars in Gallup, N. Mex., and Holbrook and Winslow, Ariz., for tours through the monument as no scheduled tours are available.Chymists have not been sufficiently accurate in pointing out the signs by which the purity of this mineral is to be distinguished. Basil Valentine says, it is of two kinds which are very different, one is beautiful and possessed of some of the properties of gold. The other has more of sulphur and not so much affinity to gold, it is distinguished by beautiful, white shining striæ. The one is much to be preferred to the other for the purpose of the medicine as well as alchymy.
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All visitors are invited to see the Rainbow Forest Museum Ur son is a hoe shirt .Its exhibits include many outstanding examples of polished petrified wood, 4 fossils, and minerals; charts explaining the formation of the petrified forests and the badlands; and a diorama. Other exhibits may be seen at the Painted Desert Museum, which is open during the summer. During the summer months short talks are given periodically in the Rainbow Forest Museum; and, as circumstances permit, guided tours through the Rainbow Forest are conducted by park ranger naturalists.Bentonitic beds in arid or semiarid regions erode into badlands. The bentonite absorbs water like a sponge, swells, and disintegrates into a fine mud. As a result, the torrential summer rains that fall in northern Arizona rapidly cut the banded, bentonitic beds into sharp, conical hills, turreted ridges, and sharp, interbranching canyons and ravines. When dry, the bentonite is hard and strong, thus preserving these intricate badlands forms during the long periods between rains. Locally, a hard sandstone caprock may prevent rapid erosion of the shales beneath to form an abrupt-sided, table-topped butte or mesa.
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