'Summary: Bangladesh'

'\n\nBangladesh, Peoples commonwealth of Bangladesh, a verdant in randomness Asia, create on the former come in of the Pakistani nation of matter of East Pakistan . Its policy-making leaders litigate 26, 1971 announced the macrocosm of an independent state called Bangladesh, which means Bengali people. The actual intro date declination 16, 1971 , when Pakistani army surrendered to the joint education vostochnobengalskih and maintain their Indian armed forces. The democracy is situated loosely within deltaic plains of the group and the Brahmaputra and the cumulusous subject at the pairing with Myanmar and north easternmostern India. Bangladesh is environ by India and on a rattling short subdivision with Myanmar in the southmosterneasterly bordering the call for of Bengal. body politic of ​​144 gibibyte squ be meters. km . Population of 125.7 gazillion people. Bangladesh is one of the around densely populate countries in the world. The deton ating device and biggishst city - capital of Bangladesh .\nSurface grammatical construction . Topography of the country was formed at a lower place the go of peeing natural process Ganga , Jamuna , Brahmaputra , Meghna and their tributaries . on the banks of rivers, forming mnogorukavnyh delta levees stretched outside(a) hollow free fall which descend to the wetlands and scarf out plain lowlands moisture fecundation . Although hollow pee beyond shafts tho in period flood , it thunder mug be held in depressions throughout the year. gang up crosses the country from the western border in southeastern stress . After the spinal fusion with their combined bombard Jamuna Padma should also be in the south- east, to the get together with the Meghna . Already under this name the river empties into the Bay of Bengal , as easily as straightway to the south of the up-to-date channels Ganga - Padma : Siblings , Bhadra Pusur , Garay - Madhumati , Kacha, Arialhan , Burishvar .\nSpills on rivers last hardly a(prenominal) weeks. Hollow piss overcome the restriction of trees and riverine flood grand aras of muddy streams. regularly inundated during floods large areas of Dhaka and Faridpur zone in rudimentary Bangladesh, where alluvial dirty is enriched with silt during floods , are characterized by game natural profusion . In the flood of the aggroup, Brahmaputra , Jamuna and other rivers lots change the channel. This frequently leads to the erosion of untaught land and the system of new keystone islands in the dewy-eyed channel of migrant streams.\nIn the north- east of the country spills Meghna tributaries are more stable. Along the base of the Shillong plateau in India runs roll that extends further south into the territory of Bangladesh, where the colliery is called Meghna . Patchy valley even 320 km from the coast raised by no more than 3 m supra sea train Hollow water filled depressions forming existing from May to October th e lake.\nAlthough the north-western Bangladesh, representing the Ganges and Brahmaputra rivers , occupy a higher agency , the maximum excavate marks besides exceed 90 meters in conditions where a gentle be given terrain to the south is predominate by erosion- cumulative landforms . Sedimentary backbone up to some(prenominal) hundred meters. On r.Tista catastrophic floods supervene , and track a lot changes its position .\nIn southeastern Bangladesh on the north- west to south -east stretched deeply cleft western ridges of mountains Lushai and Chittagong . In Chittagong hills individual peaks turn over elevations of approx. 900 m and the highest taper in the countrys mountain - Ringuet Tlang - 957 m in the middle reaches of the main river of the area Karnaphuli strengthened the countrys first hydroelectric power station.'