South Table Mountain (Colorado)
|South Table Mountain|
View looking east from the top of Lookout Mountain
|Elevation||6,338 ft (1,932 m) |
|Prominence||475 ft (145 m) |
|Isolation||1.75 mi (2.82 km) |
|Location||Jefferson County, Colorado, U.S.|
|Parent range||Front Range foothills|
|Topo map||United States Geological Survey 7.5' topographic map|
|First ascent||February 14, 1859 by George Andrew Jackson, Thomas L. Golden and members of Chicago Company|
|Easiest route||South slope via Quaker Street|
South Table Mountain is a mesa on the eastern flank of the Front Range of the Rocky Mountains of North America. Castle Rock, the 6,338-foot (1,932 m) summit of the mesa, is located on private property 0.56 miles (0.9 km) directly east (bearing 90°) of downtown Golden, Colorado, United States, in Jefferson County.
The most distinctive feature of the mesa is its nearly flat cap that is formed by ancient Paleocene lava flows. It is separated from companion North Table Mountain, which consists of the same geologic formation, by Clear Creek.
South Table Mountain is a popular scenic and recreational destination in the Denver metro area, and most of it is preserved as Jefferson County Open Space. Its landmark prominence is Castle Rock, a small higher butte that projects from the mesa's northwest end.
South Table Mountain is underlain by sedimentary rocks of the Denver Formation, which spans the interval from latest Cretaceous to early Paleocene time. An exposure of the Cretaceous-Paleogene boundary layer has been identified and documented on its slopes.
Two prominent, columnar jointed, cliff-forming lava flows form the nearly flat cap on South Table Mountain. The Ralston Dike, a body of intrusive monzonite located about 4 miles to the northwest, probably represents the volcanic vent from which the flows erupted. The flows are about 62 to 64 million years old according to radiometric dating, which places them in the early Paleocene epoch. Generally referred to as basaltic, they are classified either as latite, or as shoshonite. They contain the minerals augite, plagioclase, and olivine altered to serpentine, with accessory sanidine, orthoclase, apatite, magnetite, and biotite.
Both North and South Table Mountain are known for the wide variety of zeolite minerals  that occur in vesicles in the second flow. These include analcime, thomsonite, mesolite, chabazite, and others. Excellent specimens of Table Mountain zeolites can be seen at the nearby Colorado School of Mines Geology Museum.
In times far past, South Table Mountain was ascended and used by American Indian tribes of the region, and archaeological remains are known to exist on its top. A piece of grape shot thought to be from either Spanish explorers or fur traders was found by Arthur Lakes on the mesa top in April 1895. The earliest recorded ascents of the mesa occurred during the Colorado Gold Rush in 1859. In 1906, father and son William H. and Clyde L. Ashworth built the original Castle Rock Resort, a cafe atop Castle Rock, where visitors were taken by burro up a trail on the north flank of Castle Rock. After vandalism destroyed it in 1907, the venture was abandoned until Charles F. Quaintance revived it in 1908 with a new cafe and burro train and a road from the south slope built by Harry Hartzell. This was supplemented in 1913 with a lighthouse, dance hall and funicular incline railway to the top. Business faded with the advent of the Denver Mountain Parks, and the funicular rails were salvaged for the allied effort in World War I in 1918. The idle resort was taken over by the Ku Klux Klan during the 1920s as a major meeting and ceremonial place, during its rise to power in Colorado. The resort burned to the ground in an arson fire in 1927. During the 1910s-1920s, the city of Denver quarried gravel from the mountain's northeast alcove. In 1935, the Works Progress Administration built the Colorado Amphitheater for Camp George West on its southern side. Developers in 1957 originally wanted to build the Magic Mountain theme park at its northeastern alcove, until residents of Applewood protested and convinced them to build elsewhere. Subsequent attempts to develop or quarry the mountain including condominiums and a corporate headquarters continued through the remainder of the 20th century, and the mesa was gradually purchased or placed under easement by Jefferson County for open space. Today, much of South Table Mountain is open to the public, while southern portions are occupied by the Colorado State Patrol and National Renewable Energy Laboratory.
Although not necessarily recorded on United States Geological Survey maps, several historically named features are part of South Table Mountain:
- Castle Rock, originally known as Table Rock, a prominent butte at northwest end
- Slaughterhouse Gulch, a gulch upon its northern slope, likely named for farms once in the Coors Brewery valley
- Long Gulch, a lengthy gulch along Quaker Street on the south slope
- Crystal Springs, natural water springs in the vicinity of the head of Long Gulch
Animals known to frequent the mesa through time include rattlesnakes, coyotes, mountain sheep, cougars, deer, elk and more. Of these, most except for the mountain sheep continue to live on the mountain today. The area, along with the adjacent north table mountain, is notorious among locals for its dense population of rattlesnakes, considered to be the most dangerous wildlife in the area. Coyotes are frequently sighted in the area but tend to avoid humans. Cougars have been spotted by some hikers, but sightings are exceedingly rare. The most commonly spotted wildlife tend to be elk, deer, coyotes, and a variety of birds.
First Ascent — earliest by a person of confirmed identity was on February 14, 1859, by gold discoverer George A. Jackson, partner Thomas L. Golden and members of the Chicago Company, a gold seeking party, all of whom were hunting mountain sheep atop the mesa.
Fastest Ascent — according to the Colorado Transcript issue of September 8, 1904, the fastest ascent was disputed between David G. Dargin, climbing to top of Castle Rock in 23:55 3/5 on November 6, 1859, and Charles Wade, climbing to top of Castle Rock from starting point of Washington Avenue Bridge at Clear Creek in 23:54 1/2 around February 1861. However, according to the website www.strava.com - onto which runners download GPS data of their activities - Golden resident Andrew Terrill ran from the Washington Avenue Bridge at Clear Creek to the summit of Castle Rock in 14:59 on November 2, 2016, making this the current Fastest Known Time (FKT). 
First Automobile Ascent — by Stanley Steamer driven by George Hering with 4 passengers (including Charles F. Quaintance) and camera equipment in 1908.
Fastest Automobile Ascent — same as first automobile ascent, timed from starting point at 13th Street and Washington Avenue in 12 minutes 45 seconds, via South Golden Road and Quaker Street, proof of ascent published on front page of the Transcript showing automobile with passengers atop Castle Rock.
Helicopter Ascent — made Transcript front page during the 1970s when helicopter made a forced landing atop Castle Rock.
- List of Colorado mountain ranges
- List of Colorado mountain summits
- List of Colorado county high points
- The elevation of South Table Mountain includes an adjustment of +0.967 m (+3.17 ft) from NGVD 29 to NAVD 88.
- "South Table Mountain, Colorado". Peakbagger.com. Retrieved November 6, 2014.
- "South Table Mountain". Geographic Names Information System. United States Geological Survey. Retrieved November 6, 2014.
- Kauffman, E.G., Upchurch, G.R. Jr., and Nichols, D.J., 2005. The Cretaceous-Tertiary boundary at South Table Mountain near Golden, Colorado. In: Extinction Events in Earth History, Lecture Notes in Earth Sciences, vol. 30, p. 365-392.
- Van Horn, R. 1957. Bedrock geology of the Golden Quadrangle, Colorado. U.S. Geological Survey, Map GQ-103.
- Kile D.E., 2004. Zeolites and associated minerals from the Table Mountains near Golden, Jefferson County, Colorado. Rocks and Minerals, vol. 79, no. 4, p. 218-238.
- Bartos, P.J. 2004. Table Mountain zeolites: The Colorado School of Mines perspective. Rocks and Minerals, vol. 79, no. 4, p. 240-244.