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Description of the Silverton Quadrangle

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Description of the Silverton Quadrangle DESCRIPTION OF THE SILVERTON QUADRANGLE By Whitman Cross, Ernest Howe, and F. L. Ransome. GEOGRAPHY AND GENERAL GEOLOGY OF THE QUADRANGLE. By Whitman Cross and Ernest Howe. INTRODUCTION. line lies in the zone between 11,500 and 12,000 which has been called the Ignacio quartzite, and which is distinguished from underlying beds not feet above the sea, and large areas in the interior which, on scanty fossil evidence, has been referred only by fossil evidence, but also by an unconformity. The term San Juan region, or simply "the San are thus barren of tree growth, and support only a to the Cambrian. Following this quartzite con­ Above the red Triassic beds come other forma­ Juan," used with variable meaning by early low alpine flora on favored surfaces. formably are thin limestones and shaly strata, the tions that are correlated in general with the fresh­ explorers, and naturally with indefinite limita­ Valuable deposits of the precious metals have latter characterized by casts of cubical salt crystals, water Jurassic of other parts of Colorado, and tion during the period of settlement, is now quite been found in many parts of the San Juan region. with a total thickness of less than 100 feet. These above these comes the upper Cretaceous, from the generally applied to a large tract of mountainous Coal beds of great extent and fine quality occur beds are distinguished as the Elbert formation and Dakota to the uppermost coal-bearing member, the country in southwestern Colorado, together with along the southern base, and agricultural lands are assigned to the upper part of the Devonian, on Laramie. Below Durango the post-Laramie forma­ an undefined zone of lower country bordering it form the valley bottoms and certain of the lower the evidence of characteristic fish remains. Above tion, made up of eruptive rock debris and known on the north, west, and south. The Continental slopes adjacent to the snow-fed streams from them occurs, in conformity, a series of limestones as the "Animas beds," rests upon the Laramie, Divide traverses this area in a great bow. The the mountains. With the development of these with thin interstratified quartzites, 200 to 400 feet and is in turn overlain by the Puerco and higher principal part of the district is a deeply scored vol­ resources several important towns have been estab­ thick, known as the Ouray formation, the lower Eocene deposits. canic plateau, more than 3000 square miles in lished in sheltered valleys on all sides. Railroads and middle portions of which are characterized by Structurally, the most striking feature in the extent, drained on the north by tributaries of the encircle the group and penetrate to some of the a definite upper Devonian invertebrate fauna. present attitude of the formations described, from Gunnison RiVer, on the west by those of the mining centers of the interior. Creede, Silverton, Although these thin formations have been fol­ the base of the Paleozoic upward, is their general Dolores and San Miguel rivers, on the south by Telluride, Ouray, and Lake City, all situated in lowed for many miles up the Animas Valley, no southerly or westerly dip away from a point in the numerous branches of the San Juan, and on the mountain valleys, are thus connected with the indication of Silurian or Ordovician strata has west-central part of the San Juan Mountains. As east by the Rio Grande. All but the latter drain­ main lines of traffic.* been found there, nor any evidence of the strati- seen in the section of the .Animas Valley, all of age finds its way to the Gulf of California through The geological history of the San Juan region is graphic gap which must exist if there are no beds these formations appear to be conformable. None the Colorado River. too complex and as yet too imperfectly known to of those ages in the section. In the Uncompahgre of the various unconformities by overlap, repre­ The San Juan Mountains, as that term is now justify even an outline statement of satisfactory Valley near Ouray the Ignacio formation is lack­ sented upon the Hayden map as occurring in the understood, embrace the area bounded on the accuracy. The pre-Tertiary surface of the entire ing and the Elbert formation is not everywhere area between the Animas and San Miguel rivers, north by the generally abrupt descent to the slop­ region was completely buried by the volcanic for­ present, and at certain localities in the Silverton exist within that territory. But two great orogenic ing mesas extending for 25 miles to the canyon of mations which now cover the main area, and, while quadrangle the Ignacio is absent. These facts disturbances, not indicated in the Animas section, the Gunnison, on the west by the great plateau erosion has again exposed some of the older rocks show that the seeming conformity in the section are clearly shown on the northern slopes of the San of Colorado and Utah, on the south by the more on all sides of the volcanic complex and even in seen on the slopes of the Needle Mountains is mis­ Juan, and possibly one of them also on the south­ gradual descent to the rolling plateaus of New some of the interior valleys, the reconnaissance leading and that there is a stratigraphic break of ern side, not far east of the Animas River. A pro­ Mexico, and on the east by the broad and level observations of the Hay den and other early surveys great importance between the Ignacio and Elbert nounced unconformity exists between the Dolores San Luis Park. From this main area a broad were far too meager, and the present resurvey has formations. and older beds in the Uncompahgre Valley, while spur leads off to the southeast, losing its moun­ thus far covered too small an area, to afford solu­ The extreme upper part of the Ouray limestone the Dolores itself and all older sediments are want­ tainous character near the Colorado-New Mexico tions to many of the problems concerning the earlier contains Mississippian (lower Carboniferous) fossils ing in the plateau traversed by the Gunnison and line. The San Juan Mountains thus have a length geologic development of this most interesting field. at a few points observed in the Animas Valley. its southern tributaries east of the Uncompahgre of nearly 80 miles east and west, and a width of In view of this condition, no attempt will be On this limestone occurs a reddish calcareous shale, River, and the granites and gneisses are overlain from 25 to 40 miles north and south, and their made at this time to present a thorough review the Molas formation, containing many chert nod­ by the probable equivalent of the La Plata sand­ summits form a great group rather than a range. of San Juan geology, but in order that the sig­ ules, and some of these cherts also carry a Missis­ stone, of assumed Jurassic age. A similar condi­ In the western part of the San Juan Mountains nificance of the observations made in the Silver- sippian fauna. Thin limestone layers in the shale tion exists east of the Animas, in the drainage the topography is very rugged. There are hun­ ton, Telluride, and other quadrangles may be more contain Pennsylvanian (upper Carboniferous) fos­ of Los Pinos and Piedra rivers, according to the dreds of summits exceeding 13,000 feet in eleva­ fully appreciated, an'outline sketch of the geologic sils, so that there is evidence of the stratigraphic Hayden map, but reconnaissance observations by tion, and several which reach more than 14,000 development of the region will be given. This break following the Ouray. The Molas shales have A. C. Spencer in the Piedra Valley show that prer feet above sea level. Here, too, the bounding outline is particularly applicable to the western been found everywhere lying on the Ouray lime­ volcanic faulting may be the cause of the irregular scarps of the group are often very precipitous, part of the San Juan, for it is in the valleys of stone with but slight unconformity. There is no relations in this district. while some of the valleys in the heart of the this portion, near the mountain front, that the best known indication of the extent of the Mississippian Other periods of uplift, Erosion, or subsidence, mountains have been cut clown to 9000 feet or exposures of the older rocks may be found. formations which may have overlain the Ouray in Paleozoic or Mesozoic time, are indicated by the less above the sea. To 'the east the configuration The Animas Valley, between Silverton and the limestone, or of their character, except that the apparent absence, or slight development, of- Cam­ is less rugged, and high table-lands, of varying vicinity of Durango, shows apparently a complete basal portion must have been a cherty limestone brian, Ordovician, and Silurian sediments, the extent, represent in a measure old plateau surfaces. exposure of all formations of the San Juan, from very similar to the Ouray and grading into it. presence of remnants of the Mississippian beds, Within the bordering zone of lower country, the Archean to the Puerco formation of the Eocene, The red shales of the Molas constitute the first the local development of the fossiliferous Triassic, having a general elevation of from 6000 to 9000 inclusive. Much of this section has now been stud­ sediments of a great complex of sandstones' and and the absence of the marine Jurassic and of feet, are situated several small groups of high ied in detail, but definite correlations can not yet be fossiliferous shales and limestones, belonging to recognized equivalents of the great lower Creta­ peaks bearing special names.
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