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Pegu Range

Coordinates:20°55.3′N95°14.9′E / 20.9217°N 95.2483°E /20.9217; 95.2483
From Wikipedia, the free encyclopedia
(Redirected fromBago Yoma)
Mountain range in Myanmar
Pegu Range
ပဲခူးရိုးမ
Mount Popa
Highest point
PeakMount Popa
Elevation1,518 m (4,980 ft)
Coordinates20°55′27″N95°15′02″E / 20.92417°N 95.25056°E /20.92417; 95.25056
Dimensions
Length475 km (295 mi) N/S
Width60 km (37 mi) E/W
Geography
Pegu Range is located in Myanmar
Pegu Range
Pegu Range
Location in Myanmar
CountryBurma
Range coordinates20°55.3′N95°14.9′E / 20.9217°N 95.2483°E /20.9217; 95.2483

ThePegu Range (Burmese:ပဲခူးရိုးမ;Pegu Yoma orBago Yoma) is a range of low mountains or hills[1] and uplands[2] between theIrrawaddy and theSittaung River in centralBurma (Myanmar). The range runs fromMount Popa in the north toSinguttara Hill (Theingottara Hill) in the south. Both thePegu River and the Sittaung River originate in the Pegu Range.

High points

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Among the notable peaks or hilltops are 1,518 metres (4,980 ft) highMount Popa, astratovolcano,[3] Sinnamaung TAUNG 2,693 feet (820 m),Shwenape TAUNG 2,509 feet (765 m), TALAN TAUNG 2,050 feet (625 m), Binhontaung 2,003 feet (611 m),[4] Kodittaung 1,885 feet (575 m),[4] Phoe-Oo Taung[3] and Singguttara Hill (Theingottara Hill).[3]

Geology

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The Pegu Range consists of folded and faultedPaleogenemarine sediments combined with more recentvolcanics.[citation needed]

History

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TheShwedagon Pagoda was built sometime before 1000 A.D. on Singguttara Hill.

The Pegu Range was the original site of the 1930–1931Saya San uprising against theBritish. Saya San raised the flag of independence on Alantaung Hill nearTharrawaddy.[5]

Later the Pegu Range became a center for theCommunist Party of Burma.[6]

Ecology

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See also:Teak in Myanmar

The northern end of the Pegu merges into the BurmeseDry Belt, while in the south there is over 80 inches of rainfall a year.[7] The hills of the Pegu Range were originally heavily forested withteak and other commercially exploitable hardwoods.[1][7] The southern forests were "ironwood forests", while the central and northern forests were teak.[8] Extensive logging has caused the presentdeforestation and increased erosion in the area.[citation needed]

Notes

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  1. ^abSeekins, Donald M. (2006)Historical dictionary of Burma (Myanmar) Scarecrow Press, Lanham, Maryland,page 357,ISBN 0-8108-5476-7
  2. ^Seekins, Donald M. (2006)Historical dictionary of Burma (Myanmar) Scarecrow Press, Lanham, Maryland,page 191,ISBN 0-8108-5476-7
  3. ^abcMoore, Elizabeth H. (2007)Early landscapes of Myanmar River Books, Bangkok, page 44,ISBN 974-9863-31-3
  4. ^abtopographic map, 1:250,000Thayetmyo, Burma, NE 46-4, Series U542, United States Army Map Service, October 1959
  5. ^Ghosh, Parimal (2000)Brave men of the hills: resistance and rebellion in Burma, 1825–1932 University of Hawai'i Press, Honolulu, Hawaii,page 174,ISBN 0-8248-2207-2
  6. ^Seekins, Donald M. (2006)Historical dictionary of Burma (Myanmar) Scarecrow Press, Lanham, Maryland,page 151,ISBN 0-8108-5476-7
  7. ^abStamp, L. Dudley (1930) "Burma: An Undeveloped Monsoon Country"Geographical Review 20(1): pp.86-109, page 105
  8. ^de Terra, Hellmut (1944) "Component Geographic Factors of the Natural Regions of Burma"Annals of the Association of American Geographers 34(2): pp. 67-96, page 82
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