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Garam Chashma

Garam Chashma

FieldValue
nameGaram Chashma
native_nameگرم چشمہ
native_name_langur
settlement_typeTown
image_skylineZhiture, Garam Chashma.jpg
image_captionSpring in Garam Chashma
pushpin_mapPakistan
coordinates
subdivision_typeCountry
subdivision_namePakistan
subdivision_type1State
subdivision_name1Khyber Pakhtunkhwa
subdivision_type2District
subdivision_name2Lower Chitral
subdivision_name3Chitral
established_titleEstablished
established_date14 August 1947
government_typeMunicipal Corporation
governing_bodyGaram-Chashma-Chitral Municipal Corporation
area_footnotesMetric
area_total_km252
elevation_m2550
population_total50000
population_as_of2003
population_density_km2auto
demographics_type1Languages
demographics1_title1Spoken
demographics1_info1Khowar, Persian
timezone1PST
utc_offset1+5
postal_code_typePostal Code
postal_code17130 - 0xx
blank1_name_sec1constituency
website
Shades of Spring in the heights of Hindu Kush
Spring in Garam Chashma

Garam Chashma (literally: Hot Spring) is one of the many branch valleys of Chitral, situated in the extreme north-west of Pakistan. It is one of the highest human settlements in the Hindukush ranges with an altitude of almost 2550 meters (8389 feet). The place is known for its hot spring, which is one of the tourist attraction sites. It is also famous for its trout fish. The water flowing down through the length of the valley is famous for fishing sports. The Lotkoh River (Garam Chashma River) running down from the lofty peaks of the Hindu Kush is most suitable for the brown type of trout fish. Other features of the area include snow-covered peaks, pleasant weather, and natural springs, and more recently, has remained in the limelight for being a potential site of hydropower generation. Besides tourists, people suffering from skin diseases also visit the hot spring for treatment (not proven scientifically). It is located in the northwest of Chitral at a distance of about forty-eight kilometres by road. It shares international borders with Afghanistan being situated in the extreme northwest of Pakistan. Dorāh Pass (14,940 feet 4,554 metres) connects this part of Pakistan with [Badakhshan, the adjacent province of Afghanistan.

Hot spring

The spring water emerges from underground sulfur deposits making its temperature rise above boiling point. For the same reason, the spring is also known as Sulphur Spring. The spring is the warmest in the westward extension of the Himalayan Geothermal Belt. It emerges from leucogranites of the Hindu Kush Range that date from 20–18 Ma. Reservoir temperatures may be as high as 260 °C. It is not clear whether the circulation of deep groundwater in this region is driven by topography or by tectonic lateral stress.{{cite journal|page=75|last1=Hochstein|last2=Regenauer-Lieb|first1=M.P. |first2=K. |title=Heat generation associated with the collision of two plates: the Himalayan geothermal belt

Demography

The Khowar is the official language spoken in this valley. The population of Garam Chashma is approximately 50,000 people. Since the last census in Pakistan was conducted in 1998, there is no precise source of information in this regard. The male-to-female ratio is almost 50-50. Almost 60 percent of the population is young people. The majority religion in Garam Chashma is Ismaili Shi'ite Islam and adherence to the Aga Khan is widespread.

Languages

Khowar is the main language spoken and understood by the majority of the population. The second most spoken language is Yidgha, an Iranian language spoken by a few thousand people in Parabeg valley. A small number of people, in Gobor Valley, also speak Sheikhan-War, a dialect spoken in the Nuristan province of Afghanistan.

Gobor Valley

In addition, many people understand and some can even speak Persian. This is due to the influence of Nasir Khisraw, the eleventh-century poet and philosopher. One of his disciples had come to this part of the region and settled here permanently. He preached the Ismaili thought, hence marking the dawn of Ismailism in this part of the world. More recently, the neighbouring country, Afghanistan, was involved in the war with the USSR and as a result, a huge influx of refugees fled to this area. Since Garam Chashma was easily accessible from Badakhshan, many Afghans chose to stay and some of the refugees are still living here. This interaction with Dari speakers refreshed the memories associated with Persian.

Educational institutions

  • Aga Khan Schools (A network of schools from ECD-High School, spread across the area)
  • Government Higher Secondary School Garam Chashma
  • Government Higher Secondary School for Women, Izh, Garam Chashma
  • Community Based Degree College for Women Ovirk, Garam Chashma
  • Government High School Ovirk, Garam Chashma
  • Government Primary and Middle School (a network of schools spread across the area)
  • Pamir Public School and College, Garam Chashma
  • Al-Nasir Community Based School, Garam Chashma
  • Chamber of Commerce College, Garam Chashma
  • Injigan Ideal Public school, Garam Chashma. (Sardar Gulab)
  • Government high school for girls Murdan
  • Community school Shagrm (Murdan)
  • Government high school Parabag for boys
  • Injigan Ideal Public school Chitral, Garamchashma.

References

References

  1. Tahir Jahangir. (24 February 2005). "A Travel Companion to the Northern Areas of Pakistan". Oxford University Press.
  2. Mirza, Sana. (2 May 2016). "www.jaag.tv". www.zemtv.com.
  3. Zahiruddin. (7 March 2011). "Chitral's Garam Chashma popular for its healing touch". [[Dawn (newspaper).
  4. electricpulp.com. "CHITRAL – Encyclopaedia Iranica".
  5. "Hindu Kush {{!}} mountains, Asia".
  6. "Khowar language, alphabet and pronunciation".
  7. "Yadgha".
  8. "Khusraw, Nasir {{!}} Internet Encyclopedia of Philosophy".
  9. "Ismaili Philosophy {{!}} Internet Encyclopedia of Philosophy".
  10. "Pamir Public School & College".
Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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