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Ischigualasto Provincial Park

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(Redirected from Ischigualasto) Protected area in the San Juan Province, Argentina
Ischigualasto Provincial Park
Parque Provincial Ischigualasto
Valle de la Luna
The Submarine, wind-eroded rock formationThe Submarine, wind-eroded rock formation
Location in ArgentinaLocation in ArgentinaLocation in Argentina
LocationSan Juan Province, Argentina
Nearest citySan José de Jáchal
Coordinates30°4′S 68°0′W / 30.067°S 68.000°W / -30.067; -68.000
Area60,370 ha (233.1 sq mi)
EstablishedNovember 3, 1971 (1971-11-03)
UNESCO World Heritage Site
Official name
Ischigualasto / Talampaya Natural Parks
TypeNatural
Criteriaviii
Reference no.966
RegionLatin America and the Caribbean

Ischigualasto Provincial Park (Spanish: Parque Provincial Ischigualasto), also called Valle de la Luna ("Valley of the Moon" or "Moon Valley"), due to its moon-like appearance, is a provincial protected area in the north-east of San Juan Province, north-western Argentina, limiting to the north with the Talampaya National Park, in La Rioja Province. Both areas belong to the same geological formation, the Ischigualasto Formation (sometimes called the Ischigualasto-Talampaya Formation). Established on 3 November 1971, the park has an area of 60,370 ha (603.7 km; 233.1 sq mi).

In 2000, UNESCO included Ischigualasto and Talampaya National Park among its World Heritage Sites.

History

The name Ischigualasto is derived from the extinct Cacán language, spoken by an indigenous group referred to as the Diaguita by the Spanish conquistadors and means "place where the moon alights". Another hypothesis gives the name "Ischigualasto" a Quechua origin, meaning "dead land", although some scholars have proposed Huarpe roots.

The first paleontological description of Ischigualasto dates from 1930. In 1941 the area was studied in more detail, which led to the discovery of 70 species of fossil plants. The region received for the first time the name Valle de la Luna in 1943, in a publication edited by the Automobil Club Argentino. That year, Dr. Ángel Cabrera of University of La Plata described the traversodontid Exaeretodon—the first cynodont found in Ischigualasto—after samples sent by a geologist prospecting for coal on behalf of an Argentine mining company.

Academic work and geological prospecting proceeded slowly until 1958, when Dr. Alfred Sherwood Romer, a Harvard University expert in ancient mammals, discovered several rich fossil beds which he described as "extraordinary".

Description

Most of the park lies within the Valle Fértil Department, with a minor part in the Jachal Department of San Juan, at an altitude of about 1,300 m (4,300 ft) amsl. The park is part of the western border of the Central Sierras, and features typical desert vegetation (bushes, cacti and some trees) which covers between 10 and 20% of the area. The climate is very dry, with rainfall mostly during the summer, and temperature extremes (minimum −10 °C or 14 °F, maximum 45 °C or 113 °F). There is a constant southern wind with a speed of 20–40 km/h (12–25 mph) after noon and until the evening, sometimes accompanied by the extremely strong Zonda wind.

  • Ischigualasto Provincial Park scenery
  • Las Coloradas cliff Las Coloradas cliff
  • Water-eroded badlands Water-eroded badlands
  • The Sphynx, wind-eroded rock formation The Sphynx, wind-eroded rock formation
  • The Mushroom, wind-eroded rock formation The Mushroom, wind-eroded rock formation

Paleontology

Main articles: Ischigualasto Formation and Ischigualasto-Villa Unión Basin See also: Choiyoi Group
Fauna of the Ischigualasto Formation
Fossil discovered in Ischigualasto National Park

The Ischigualasto Formation contains Late Triassic (Carnian) deposits (231.4 -225.9 million years before the present), with some of the oldest known dinosaur remains, which are the world's foremost with regards to quality, number and importance.

In the Carnian this area was a volcanically active floodplain dominated by rivers and had a strongly seasonal rainfall. Petrified tree trunks of Protojuniperoxylon ischigualastianus more than 40 m (130 ft) tall attest to a rich vegetation at that time. Fossil ferns and horsetails have also been found.

Rhynchosaurs and cynodonts (especially rhynchosaur Hyperodapedon and cynodont Exaeretodon) are by far the predominant findings among the tetrapod fossils in the park. A study from 1993 found dinosaur specimens to comprise only 6% of the total tetrapod sample; subsequent discoveries increased this number to approximately 11% of all findings. Carnivorous dinosaurs are the most common terrestrial carnivores of the Ischigualasto Formation, with herrerasaurids comprising 72% of all recovered terrestrial carnivores. Dinosaurs of Ischigualasto Formation include early samples of the two major lineages of dinosaurs (ornithischians and saurischians). The carnivorous archosaur Herrerasaurus is the most numerous of these dinosaur fossils. Another important putative dinosaur with primitive characteristics is Eoraptor lunensis, found in Ischigualasto in the early 1990s.

See also

References

  1. ^ Ley No. 3666 de la Provincia de San Juan, 11 de noviembre de 1971; sanc.: 3 de noviembre de 1971
  2. ^ "Ischigualasto / Talampaya Natural Parks". UNESCO World Heritage Centre.
  3. (in Spanish) El lugar donde se posa la luna
  4. Cabrera 1943.
  5. ആകാശത്ത് മാത്രമല്ല ഭൂമിയിലും ചന്ദ്രനുണ്ട്: വിചിത്ര കാഴ്ചകൾ നിറഞ്ഞ 'ചന്ദ്രന്‍റെ താഴ്‌‌‌വര' [The moon is not only in the sky but also on earth: the 'valley of the moon' full of strange sights...;]. ManoramaOnline (in Malayalam). Retrieved 2021-09-09.
  6. ^ Martínez et al. 2011.
  7. Rogers et al. 1993.

Bibliography

External links

World Heritage Sites in Argentina
Northwest Argentina
Mesopotamia
Cuyo
Pampas
Patagonia
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