কুমায়ূন বিভাগ: সংশোধিত সংস্করণের মধ্যে পার্থক্য

বিষয়বস্তু বিয়োগ হয়েছে বিষয়বস্তু যোগ হয়েছে
সম্পাদনা সারাংশ নেই
ট্যাগ: মোবাইল সম্পাদনা মোবাইল ওয়েব সম্পাদনা উচ্চতর মোবাইল সম্পাদনা
সম্পাদনা সারাংশ নেই
ট্যাগ: মোবাইল সম্পাদনা মোবাইল ওয়েব সম্পাদনা উচ্চতর মোবাইল সম্পাদনা
৬ নং লাইন:
এটি [[ভারতীয় সেনাবাহিনী]]র [[কুমায়ুন রেজিমেন্ট|কুমায়ূন রেজিমেন্টের]] প্রধান স্থান।
কুমায়ূনের গুরুত্বপূর্ণ ও বিখ্যাত শহরগুলি হল; [[নৈনিতাল]], [[আলমোড়া]], [[পিথোরাগড়]], [[চম্পাবত]], [[বাগেশ্বর]] এবং [[রানীক্ষেত]]। [[নৈনিতাল]] হল কুমায়ুন বিভাগের প্রশাসনিক দপ্তর এবং উত্তরাখণ্ড হাইকোর্টটিও এই শহরেই অবস্থিত।<ref>[http://indiaguide.trailofview.com/trail/Traveling_in_Kumaon Kumaon Information]{{dead link|date=December 2017 |bot=InternetArchiveBot |fix-attempted=yes }}</ref>
 
== ভূগোল ==
[[File:Trishul peak in the golden hour.jpg|alt=|thumb|right|287x287px|[[ত্রিশূল পর্বত]]]]
[[File:Dream_country.jpg|alt=|কুমায়ূন হিমালয় পর্বতমালা, [[কৌশানী]]|thumb|250x250px]]
[[File:Nainital Lake, April, 2009.JPG|thumb|[[নৈনিতাল হ্রদ]], কুমায়ূনের চারটি হ্রদের মধ্যে একটি]]
[[File:Kosi River valley near Almora, Uttarakhand, India.jpg|thumb|কুমায়ূনের [[আলমোড়া]]র নিকট [[কোশী নদী]]র উপত্যকা]]
The Kumaon<ref>{{Cite web|url=https://www.indiavacationspots.com/kumaon-garhwal-vacation-tour/|title=Garhwal Vacation Tips - Vacation Tour Garhwal Kumaon -Family Tour India}}</ref> region consists of a large [[Himalayas|Himalayan]] tract, together with two [[wikt:submontane|submontane]] strips called the [[Terai]] and the [[Bhabar]]. The submontane strips were up to 1850 an almost impenetrable forest, given up to wild animals; but after 1850 the numerous clearings attracted a large population from the hills, who cultivated the rich soil during the hot and cold seasons, returning to the hills in the rains. The rest of Kumaon is a maze of mountains, part of the [[Himalaya]] range, some of which are among the loftiest known. In a tract not more than 225&nbsp;km in length and 65&nbsp;km in breadth there are over thirty peaks rising to elevations exceeding 5500 m.<ref name=EB1911>{{EB1911 |wstitle=Kumaon |volume=15 |page=945 |inline=1}}</ref>
 
The rivers like [[Gori River|Gori]], Dhauli, and [[Kali River (Uttarakhand)|Kali]] rise chiefly in the southern slope of the [[Tibet]]an watershed north of the loftiest peaks, amongst which they make their way down valleys of rapid declivity and extraordinary depth. The principal is the [[Sharda River|Sharda]] (Kali Ganga), the [[Pindari Glacier|Pindari]] and Kailganga, whose waters join the [[Alaknanda River|Alaknanda]].<ref name=EB1911/> The river Sharda (Kali Ganga) forms the international boundary between India and Nepal. The pilgrim route currently used to visit [[Mount Kailash|Kailash-Mansarovar]] goes along this river and crosses into [[Tibet]] at [[Lipulekh Pass|Lipu Lekh pass]].
 
The chief trees are the [[Chir Pine]], [[Cupressus|Himalayan Cypress]], [[fir|Pindrow Fir]], [[Alder]], [[Sal tree|Sal]] and Saindan. [[Limestone]], [[sandstone]], [[slate]], [[gneiss]] and [[granite]] constitute the principal geological formations. Mines of [[iron]], [[copper]], [[gypsum]], [[lead]] and [[asbestos]] exist; but they are not thoroughly worked. Except in the submontane strips and deep valleys, the climate is mild. The rainfall of the outer Himalayan range, which is first struck by the monsoon, is double that of the central hills, in the average proportion of 2000&nbsp;mm to 1000&nbsp;mm. No winter passes without snow on the higher ridges, and in some years, it is universal throughout the mountain tract. Frosts, especially in the valleys, are often severe.<ref name=EB1911/>
 
==তথ্যসূত্র==