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trusted in myself, but on this particular one I was so disgusted that I had made up my mind to trust in Providence alone. I did well, for had I done otherwise I might have fared much worse than I did. We went over a pass (elev. 2,400 ft.) between two small domes, quite barren but for a scanty growth of short dried grass. We were marching over masses of lava and conglomerate with innumerable marble pellets. We found ourselves within a regular circle of low hills enclosing a shallow depression. Subsequently we came to a second and then to a third similar depression. [Illustration: Author's Caravan marching across Trailless Country.] [Illustration: The Roncador River.] Continuing in a north-westerly direction we again obtained a gorgeous view of the treble _portal_--by which word the Brazilians describe a monumental entrance of any kind. That is just what those three immense gaps in the plateau looked like: an immense wall of rock forming a high barrier, with three gigantic natural gateways. After finding a stream of good water on the west side of the plateau we rose again higher, obtaining a splendid bird's-eye view of the picturesque depression we had just crossed. The effects of erosion following those of volcanic activity were evident enough upon the entire landscape. On the west side we had a horseshoe-shaped vertical wall--seemingly containing an extinct crater--and yet another on the north side of the western end of the elongated ellipse which was there formed. With some difficulty we managed to get the animals up to the summit of the plateau (elev. 2,580 ft.). From there we obtained a sumptuous view beyond. An immense dyke of brilliant red rock, flat-topped, lay majestically to the west. At its foot the Rio Pedra Grande had its birth, and then flowed westward into the Rio Roncador. Four gigantic flat table-lands stood impressively in a line. Three more, equally impressive, loomed in the south-west. Other minor ones, quite wall-like--rectangular in vertical section--appeared in the blue distance, while the horizon was barred by a long flat plateau. Looking north as we descended from the table-land, we found on our left another extinct crater--semicircular in shape, with several superimposed strata of lava, each about one foot thick, capping its lip, which was broken up into three sections. The valley below that crater formed a _cuvette_, the bottom of which (elev. 2,200 ft.) showed deep erosion by w
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