| Soda Dam Hot Spring | |
|---|---|
| Soda Dam Jemez Springs Soda Dam | |
 | |
 | |
| Location | near the town of Jemez Springs, NM |
| Coordinates | 35°47′40″N106°41′12″W / 35.79445°N 106.68669°W |
| Elevation | 6,332 feet |
| Type | volcanic |
| Temperature | 117°F (47°C) |
The Soda Dam Hot Spring, also known as the Jemez Springs Soda Dam or simply Soda Dam, is a grouping of fifteen hot springs which have formed a unique calcium carbonate and travertine formation creating a bridge over the Jemez River in Northern New Mexico. [1] [2]
The Soda Dam was formed by calcium carbonate and travertine deposits from the thermal spring water that was built up over the course of 7,000 years. The river flows through the dome-like bridge created by the deposition of these minerals across the river. There is also a waterfall at the site, over 300 feet long, 50 feet high, and 50 feet wide at the base. [1] [3]
The hot spring water is heated by volcanic magma of the Valles Caldera. The water percolates through shale and limestone, following cracks in the Jemez geological fault zone to emerge at the springs. Because algal filaments are contained within the carbonate rock, the site is used to study ways in which possible ancient life on Mars may be detected through examination of rocks. [4] The hot spring water emerges from several sources and seeps. [5]
When State Highway 4 was built, part of the travertine dam was removed. The remaining portion is East of the highway. [5]
The springs were used by local indigenous people before the arrival of settlers. Artifacts and archaeological finds have been discovered at Jemez Cave near Soda Dam; evidence of human use as long ago as 2,500 B.C. [6] In addition to the cave, several rock shelters can be found in the area. In the 1930s, extensive archaeological materials were found in the area around Soda Dam, and it was determined that the area has been used for over 2,000 years by several cultures. [5]
In the 1960s, New Mexico state highway #4 was built which involved blasting the rock to build the road. The course of the spring water changed at that time, and now most of it flows into ditches on either side of the road. [7] Some of the springs stopped flowing entirely. [1]
The maximum water temperature of the spring system is 117 °F (47 °C). [8] [9]
The geographic coordinates are N 35.79445 W 106.68669. [10]
The geothermal areas of Yellowstone include several geyser basins in Yellowstone National Park as well as other geothermal features such as hot springs, mud pots, and fumaroles. The number of thermal features in Yellowstone is estimated at 10,000. A study that was completed in 2011 found that a total of 1,283 geysers have erupted in Yellowstone, 465 of which are active during an average year. These are distributed among nine geyser basins, with a few geysers found in smaller thermal areas throughout the Park. The number of geysers in each geyser basin are as follows: Upper Geyser Basin (410), Midway Geyser Basin (59), Lower Geyser Basin (283), Norris Geyser Basin (193), West Thumb Geyser Basin (84), Gibbon Geyser Basin (24), Lone Star Geyser Basin (21), Shoshone Geyser Basin (107), Heart Lake Geyser Basin (69), other areas (33). Although famous large geysers like Old Faithful are part of the total, most of Yellowstone's geysers are small, erupting to only a foot or two. The hydrothermal system that supplies the geysers with hot water sits within an ancient active caldera. Many of the thermal features in Yellowstone build up sinter, geyserite, or travertine deposits around and within them.
Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate. Because of the huge amount of geothermal vents, travertine flourishes. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas.
Travertine is a form of terrestrial limestone deposited around mineral springs, especially hot springs. It often has a fibrous or concentric appearance and exists in white, tan, cream-colored, and rusty varieties. It is formed by a process of rapid precipitation of calcium carbonate, often at the mouth of a hot spring or in a limestone cave. In the latter, it can form stalactites, stalagmites, and other speleothems. It is frequently used in Italy and elsewhere as a building material. Similar deposits formed from ambient-temperature water are known as tufa.
Valles Caldera is a 13.7-mile (22.0 km) wide volcanic caldera in the Jemez Mountains of northern New Mexico. Hot springs, streams, fumaroles, natural gas seeps and volcanic domes dot the caldera floor landscape. The highest point in the caldera is Redondo Peak, an 11,253-foot (3,430 m) resurgent lava dome located entirely within the caldera. Also within the caldera are several grass valleys, or valles, the largest of which is Valle Grande, the only one accessible by a paved road. In 1975, Valles Caldera was designated as a National Natural Landmark by the National Park Service with much of the caldera being within the Valles Caldera National Preserve, a unit of the National Park System.
Pamukkale, meaning "cotton castle" in Turkish, is a natural site in Denizli Province in southwestern Turkey. The area is famous for a carbonate mineral left by the flowing of thermal spring water. It is located in Turkey's Inner Aegean region, in the River Menderes valley, which has a temperate climate for most of the year.
Mineral springs are naturally occurring springs that produce hard water, water that contains dissolved minerals. Salts, sulfur compounds, and gases are among the substances that can be dissolved in the spring water during its passage underground. In this they are unlike sweet springs, which produce soft water with no noticeable dissolved gasses. The dissolved minerals may alter the water's taste. Mineral water obtained from mineral springs, and the precipitated salts such as Epsom salt have long been important commercial products.
The Jemez Mountains are a group of mountains in Rio Arriba, Sandoval, and Los Alamos counties, New Mexico, United States.
The Santa Fe National Forest is a protected national forest in northern New Mexico in the Southwestern United States. It was established in 1915 and covers 1,558,452 acres (6,306.83 km2). Elevations range from 5,300 feet (1600 m) to 13,103 feet (4000 m) at the summit of Truchas Peak, located within the Pecos Wilderness. The Jemez, Coyote, and Cuba districts are located in the Jemez Mountains; the Pecos/Las Vegas district is located in the Sangre de Cristo Mountains; and the Española district is located in both mountain ranges. In descending order of land area the forest lies in parts of Rio Arriba, San Miguel, Sandoval, Santa Fe, Mora, and Los Alamos counties. Forest headquarters are located in the city of Santa Fe.
Hierve el Agua is a set of natural travertine rock formations in San Lorenzo Albarradas, Oaxaca, Mexico that resemble cascades of water. The site is located about 70 km east of Oaxaca City, and consists of two rock shelves or cliffs which rise between fifty and ninety metres from the valley below, from which extend nearly white rock formations which look like waterfalls. These formations are created by fresh water springs, whose water is over-saturated with calcium carbonate and other minerals. As the water trickles over the cliffs, the excess minerals are deposited, much in the same manner that stalactites are formed in caves. One of the cliffs, called the "cascada chica" or the Amphitheatre, contains two large artificial pools for swimming as well as a number of small natural pools. One of the artificial pools is very near the edge of the cliff.
The Jemez River is a tributary of the Rio Grande in eastern Sandoval County, New Mexico, United States.
Badab Soort is a natural site in Mazandaran Province in northern Iran, 95 kilometres (59 mi) south-east of the city of Sari, and 7 kilometres (4.3 mi) east of Orost village. It comprises a range of stepped travertine terrace formations that have been created over thousands of years as flowing water from two mineral hot springs cooled and deposited carbonate minerals on the mountainside.
Travertine Hot Springs are a group of geothermal mineral springs located near the town of Bridgeport, California.
The Bandelier Tuff is a geologic formation exposed in and around the Jemez Mountains of northern New Mexico. It has a radiometric age of 1.85 to 1.25 million years, corresponding to the Pleistocene epoch. The tuff was erupted in a series of at least three caldera eruptions in the central Jemez Mountains.
The Keres Group is a group of geologic formations exposed in and around the Jemez Mountains of northern New Mexico. Radiometric dating gives it an age of 13 to 6 million years, corresponding to the Miocene epoch.
The Tewa Group is a group of geologic formations exposed in and around the Jemez Mountains of northern New Mexico. Radiometric dating gives it an age of 1.85 million to 72 thousand years, corresponding to the Pleistocene epoch.
Spence Hot Springs are a group of geothermal springs located north of the town of Jemez Springs, New Mexico, in the Valles Caldera National Preserve.
McCauley Hot Springs, also known as McCauley Warm Springs is a thermal spring in the Santa Fe National Forest, near the Jemez Springs area of Northern New Mexico.
San Antonio Hot Springs are a group of geothermal springs located in the Santa Fe National Forest in Northern New Mexico.