Göreme Historical National Park (pronounced [ˈɟœɾeme]; Turkish: Göreme Tarihî Milli Parkı) is a national park in central Turkey. It occupies an area of nearly 100 km2 (39 sq mi) and is located in Nevşehir Province. It became a UNESCO World Heritage Site in 1985 under the name Goreme National Park and the Rock Sites of Cappadocia. The park features a rocky, water- and wind-eroded landscape with a network of ancient, interconnecting underground settlements.[1]
| Göreme Historical National Park | |
|---|---|
| Göreme Tarihî Millî Parkı | |
 | |
  Göreme Historical National Park | |
| Location | Nevşehir Province, Turkey |
| Coordinates | 38°39′10″N 34°51′47″E / 38.65278°N 34.86306°E |
| Area | 9,884 ha (24,420 acres) |
| Website | Website |
| Official name | Göreme Historical National Park and the Rock Sites of Cappadocia |
| Type | Mixed |
| Criteria | i, iii, v, vii |
| Designated | 1985 (9th session) |
| Reference no. | 357 |
| Region | Western Asia |
Description
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The National Park is located in the volcanic region of Mount Hasan and Mount Erciyes in Central Anatolia, in the vicinity of Ürgüp, Çavuşin and Göreme. The park area consists of plateaus and high hills, dissected by streams and river valleys carved out by the water, the valleys having steeply sloping sides. Part of this rugged area consists of basalt and thick beds of tuff. The tuff is the result of ash emitted from volcanoes millions of years ago, which solidified into soft rock, and has since been overlain by solidified lava which forms a protective capping. This has been eroded over the millennia to form the multi-coloured cliffs, rock towers, pillars, tent rocks and fairy chimney rock formations present in the park. Love Valley is known for its fairy chimneys. [1][2] This area experiences annual precipitation of 380 mm (15 in) and there is little vegetation except in riverine corridors.[3]
The earliest signs of monastic activity in Cappadocia can be traced back to the 4th century when small anchorite communities, following the teachings of Basileios the Great, Bishop of Kayseri, started to inhabit the cells hewn in the rock. Later, the communities took refuge together in underground villages to avoid attacks by marauding Arabs.[4]
Underground dwellings
editPeople have made use of the soft tuff rock to hollow out underground dwellings. The earliest monastic activity in Cappadocia is thought to have been in the fourth century when anchorites started hewing out cells from the rock. To resist Arab marauders, they linked these cells and created underground communities, with chapels, store rooms, and living quarters. Villages and small towns were developed in this way, and by 842, underground churches were being richly decorated with coloured paintings.[5]
Nowadays people don't live far underground as in the past when they were hiding or fleeing enemies. But some people still live in cave dwellings that have been made into homes, with a door/opening to daylight at ground level. Unfortunately, it has been found that long-term cave dwellers experience an unexpectedly high incidence of mesothelioma, a form of cancer. This has been linked to the inhalation of erionite fibres, a mineral common in tuff formations.[3][6][7]
References
edit- ^ a b "Goreme (Göreme) Historical National Park". National Parks of Turkey. Retrieved 27 April 2019.
- ^ "Goreme National Park and the Rock Sites of Cappadocia". Natural World Heritage Sites. Retrieved 27 April 2019.
- ^ a b "Goreme National Park, Turkey". Nasa Earth Observatory. 7 June 2009. Retrieved 27 April 2019.
- ^ "Göreme National Park and the Rock Sites of Cappadocia". UNESCO. Retrieved 12 June 2019.
- ^ "Goreme National Park and the Rock Sites of Cappadocia". UNESCO. 7 June 2009. Retrieved 27 April 2019.
- ^ Bangham, Jenny (July 2006). "Epidemiology - A rock and a hard place" (PDF). Nature Reviews Cancer. 6 (7): 489. doi:10.1038/nrc1941. ISSN 1474-1768. Retrieved 14 August 2024.
- ^ Dogan, A. U. (2006). "Genetic predisposition to fiber carcinogenesis causes a mesothelioma epidemic in Turkey". Cancer Research. 66 (10): 5063–5068. doi:10.1158/0008-5472.CAN-05-4642. ISSN 1538-7445. PMID 16707428. Retrieved 14 August 2024.