bhoda.] GEOGRAPHY HEAD OF UNCOMPAHGRE RIVER. 475 



On our return to Howardville we rode across the rolling ground which 

 extends southward from Cunningham Pass. Arriving at the town, we 

 found Mr. Jackson, the photographer of the expedition, with his party. 

 He had just arrived from the Los Pinos agency. We made the ascent 

 of Sultan Mountain with him, and he succeeded in getting a number of 

 good photographs of the surrounding country. From this point is ob- 

 tained by far the best view of Bakers Park that is obtainable from auy 

 peak in the vicinity. 



After getting our supplies we marched up Mineral Creek, while Mr. 

 Jackson struck south over the trail which passed around the west side 

 of Sultan Mountain, and made a very interesting investigation of the 

 old ruins in Southwestern Colorado. 



In the afternoon rain fell, and continued into the night, but the next 

 morning was cold and the sky clear and beautiful. This date (Septem- 

 ber 3) is remarkable as beiug the time of the abrupt change between 

 summer and fall. After this, till the snow-storms commenced, the 

 weather was cold and clear. Having camped overnight at the 

 junction of Bear and Mineral Creeks, the next morning we moved 

 up the latter, and made stations 27 and 28 on a high ridge between 

 Mineral and Cement Creeks. Camping near the head of the creek, 

 the following day we crossed the pass at its head and passed over 

 to the head of the Uncompahgre Eiver. The elevation of this 

 pass is 11,100 feet above the sea. It is entirely covered with timber. 

 The slope to the south is quite gradual, but to the north, down the 

 Uncompahgre, the fall is 800 feet in two miles. Then for several miles 

 the stream flows comparatively smoothly, till it finally enters a deep 

 box-canon, where the fall is very great. Traveling for some distance is 

 both difficult and dangerous. At the bottom of the first steep slope a 

 great area of fallen timber commences. The logs so cover the ground 

 that traveling is very nearly impossible. Leaving a notice for the pack- 

 train to camp near the beginning of this dead timber, Mr. Wilson, Dr. 

 Endlich, and I rode on, and finally got through the timber, when we 

 had open grassy ground to travel over, but the slope was so steep that 

 we could ride only a small part of the way. Leaving our mules loose, 

 as usual, to find what grass they might at this elevation, which 

 was a little less than 13,000 feet, we made station 29, on a round-topped 

 peak, which, being surrounded by peaks higher than itself, is of no great 

 importance. It was taken as a station, because its position between two 

 of the main branches of the Uncompahgre made it a key-point for the 

 drainage system which forms the head of that stream. Its elevation 

 is 13,200 feet. Prom this point we got by far the best view of Mount Snef- 

 fels, and the curious pinnacle-forms in its vicinity, which have already 

 been mentioned as seen from station 10. The accompanying illustration, 

 taken trom a hasty topographical sketch, will give a taint idea of the 

 great peak and its vicinity. Of course the elevation and ruggedness of 

 the mountains shown in the sketch can only be appreciated by a per- 

 son who has climbed many mountains. Even then the air is so clear at 

 these high altitudes that one is deceived in spite of himself with regard 

 to distances. From here we could see no feasible route by which to 

 climb the great Mount Sneffels, so we laid the question aside till a view 

 from some peak farther to the west should solve it satisfactorily. Next 

 day we retraced our steps over the pass and down Mineral Creek, camp- 

 ing agaiu at its junction with Bear Creek. Moving up the latter stream, 

 we camped on a considerable branch which comes in from the north. 

 This is probably the fiuest camping-ground on the whole stream, with 

 fine timber, good water, and a sufficient quantity of grass. Above this 



