May 12. 2006
We had to get up early because we had long ways to go all the way to Utah. First we stopped at the Florissant fossil beds.
Fossils of Ancient Lake Florissant
After Florissant we were heading toward the Black Canyon of the Gunnison.
We stopped at Gunnison for lunch and after that the area become very beautiful.
Soon we arrived to the Black canyon of the Gunnison.
"The Black Canyon of the Gunnison is one of the most striking canyons in the world. It is extremely deep and tight. Depth varies from about 1,730 to 2,420 feet, some places it is only 1,300 feet from north to south rim. It was formed by the erosive action of the Gunnison River cutting into the Precambrian rocks. A tectonic event called the "Mid Tertiary uplift" had a major part in the canyon's creation. This widespread uplift which affected the whole Rocky Mt. region and happened about 28 million years ago, and become even more accelerated about 10 million years ago. During this tectonic activity, instead of major upward movement by individual blocks, the whole Colorado region gained about 5000 feet in elevation. This resulted in regional stream down-cutting and erosion. The Mid Tertiary Uplift event was accompanied by volcanic activity also. The Gunnison River had its course altered by lava flows and ash falls to its north in the present-day West Elk Mts. area. As volcanic activity died out, the river had relatively soft volcanic rocks to erode away and to establish its course through. The last work of the vertical downcutting through the tough Precambrian rocks probably occurred over the last 2 million years. Glacial melt-offs during this period would not only furnish the water necessary to make the most of the erosive potential created by the regional uplift, but the rock debris to mechanically assist the process. Perhaps once the Gunnison had managed to cut down a little ways into the hard Precambrian rocks, it was entrenched by the resistant rocks and couldn't laterally change course. Vertical fractures in the Precambrian rocks might have influenced how things developed. The Precambrian rocks you see in the Canyon fall into two basic groups. The oldest is a strongly deformed gneiss unit, dated at around 1.7 to 1.8 billion years in age. The other major group is igneous intrusive granite dated at about 1.4 billion years. "
After our hike and some swimming (temperatere was about 55F)in the river of the Black canyon of the Gunnison we started our trip to Telluride. It is a very beautiful place with lots of geology and historic gold mines.
On the way to Telluride (14 thouseners in the fore ground)
"Telluride is the bridge from the frontier to the beginnings of the modern world. Nestled in a picturesque mountain valley and surrounded by cliffs and peaks sculpted to perfection, Telluride was the scene of many encounters that the mining frontier had with its own destiny. From its struggle to end its isolation and connect with the modern world to its mines' never-ending search for better ore-processing technology, Telluride was linked to the full bloom of the industrial revolution. Here the forces of capitalism and socialism clashed in turn-of-the-nineteenth-century labor disputes, while men wired up and harnessed the power of electricity to run not only the district's mines but also the town's street lights. And here, too, the goals of frontier precious-metal mining shifted in mid-twentieth century as the quest for base metals became a part of this country's struggle with several foreign powers.
Visitors come to Telluride to look at the ruins and rocks. The ruins among the peaks, resulting from 125 years of mining, are still capable of inspiring wonder at the inventiveness of the mining men and road builders, and the rocks and waterfalls demand the visitor's attention because of their beauty. The stories of the mining days intrigue us all. On top of that, the district has produced some fine mineral specimens.
The Telluride district rises out of the San Miguel River valley, climbing up sheer cliffs of sedimentary rock, beginning with the lowermost red sandstone of the Dolores Formation (Triassic age) to the unconformity below the Telluride Conglomerate. This unconformity represents a 30-million-year episode of uplift and erosion lasting from about 75 million years ago in the Cretaceous Period to about 45 million years ago in the Eocene Epoch. The reddish-brown to reddish-gray Telluride Conglomerate is composed of rock fragments from the eroded formations. The amount of previously deposited rock that was removed during this erosion varies greatly from place to place in the southwestern San Juan Mountains, but it is always impressive. As one travels east up the valley of the San Miguel River, the conglomerate can be seen resting on progressively older strata, beginning at the Cretaceous-aged Mancos Shale west of town and finally resting on the Triassic-aged Dolores Formation at Ingram Falls. Here the erosional surface represents the removal of some 7,000 feet of rock. The Telluride Conglomerate is the most important host rock for the base-metal replacement deposits of the Telluride district (Purington 1898; Cross and Purington 1899; Luedke and Burbank 1963; Burbank and Luedke 1966; Molenaar 1968; Fisher 1990). (http://www.findarticles.com/p/articles/mi_m0GDX/is_5_75/ai_65277661)
After Telluride we started our way toward the deserts of Utah. On the way we saw some incredible geology sites and an even more stunning moon rise.
We arrived to Moab relatively late, and wanted to go to Arches for the sunrise so went to bed soon.