Array
(
[0] => Array
(
[name] => {:en}Jaflong{:}{:bn}জাফলং{:}
[post_id] => 4142
[post_link] => http://offroadbangladesh.com/bn/places/jaflong/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/03/800-Jaflong_Sylhet_Shahnoor-Habib-Munmun1-300x225.jpg
[post_content] => {:en}
Jaflong is a union situated at Bangladesh-India border. Jaflong is a landscape beauty among gardens and hills. It is situated next to the river Peain round Hill Khashia. The Mari River originating from the great Himalayas brings tons of stone slabs with its stream. It’s a hilly area comprising of green forests.
Jaflong is a hill station and popular tourist destination in the Division of Sylhet, Bangladesh. It is located in Gowainghat Upazila of Sylhet District and situated at the border between Bangladesh and the Indian state of Meghalaya, overshadowed by subtropical mountains and rainforests. Jaflong is famous for its stone collections and is home of the Khasi (also known as Khasia) tribe.
Jaflong is one of the most attractive tourist spots in Sylhet division. It is about 60 km from Sylhet town and takes two hours drive to reach there. Jaflong is also a scenic spot nearby amidst tea gardens and rare beauty of rolling stones from hills. It is situated besides the river Mari in the lap of Hill Khashia.
{:}{:bn}
বাংলাদেশ-ভারতের সীমান্তবর্তী খাসিয়া পাহাড়ের কোলে মারি নদীর পাশে অবস্থিত পাহাড়, সবুজ বন ও বাগানের সৌন্দর্য ঘেরা একটি পাহাড়ি অঞ্চলের নাম জাফলং। হিমালয় থেকে সৃষ্ট মারি নদী এখানে প্রচুর পরিমানে পাথরখণ্ড বয়ে নিয়ে আসে।
জাফলং হল সিলেট বিভাগের একটি হিল স্টেশন এবং অন্যতম আকর্ষণীয় পর্যটন কেন্দ্র। সিলেট শহর থেকে ৬০ কিলোমিটার দূরে অবস্থিত এই পর্যটন কেন্দ্রে সড়কপথে পৌছাতে প্রায় দুই ঘণ্টা সময় লাগে। পাথর সংগ্রহ করা এবং আদিবাসী খাসিয়া সম্প্রদায়ের বসবাস এই দুটি কারনে জাফলং এর খ্যাতি রয়েছে। চা বাগান এবং পাহাড় থেকে গড়িয়ে আসা পাথরের বিরল সৌন্দর্যের দেখা মিলবে এখানে।
{:}
)
[1] => Array
(
[name] => Maharajar Dighi
[post_id] => 3086
[post_link] => http://offroadbangladesh.com/bn/places/maharajar-dighi/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/02/Moharajar-Dighi-300x200-300x200.jpg
[post_content] =>
Away from panchagar town about 10 miles a big pond is situated at Amarkhana unionis popularly known as Maharajar dighi. With the bank its surface is 800 yard. Local people says that its depth is 40 feet. Its water is clear. It has 10 saghata.It is imagined that Pitthu king dag this lake. It is said that the king attacked by a lower class and suicide with family and wealth by jumping in this lake. Every year Boishakhi fair held at the bank of the river. Many time the presence of the Indian people also seen. Beside the lake there are many green designs of trees which is very dear to all till now.
)
[2] => Array
(
[name] => {:en}Pocha Dighi and Ghora Dighi{:}{:bn}পচাদীঘি এবং ঘোড়াদীঘি{:}
[post_id] => 1567
[post_link] => http://offroadbangladesh.com/bn/places/pocha-dighi-ghora-dighi/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/02/Poocha-Dighi2-300x225.jpg
[post_content] => {:en}
Pocha Dighi and Ghora Dighi have own historical and religious significance toward the villagers. The crocodiles in the pond never will harm you even if you touch them. Here many people used to come every day in a way to make their wish fulfilled. As a result many gifts were given by them. The belief of them is high with that. So many wish have already been fulfilled. There used be a fair in almost every day. Different types of local items can be found here to shop.
[This spot needs more detail. If you have more information and photos, please be advised to add in our website. Your name will be published as a Content Contributor]
{:}{:bn}স্থানীয় গ্রামবাসীদের কাছে এই পচাদীঘি এবং ঘোড়াদীঘি দুটোরই ধর্মীয় এবং ঐতিহাসিক তাৎপর্য রয়েছে। এই দীঘির কুমিরগুলোকে স্পর্শ করলেও এগুলো আপনার ক্ষতি করবে না। এখানে প্রতিদিন অনেক মানুষ আসেন তাদের ইচ্ছা পূরণের জন্য এবং সেজন্য তারা অনেক উপহারও প্রদান করেন। ইচ্ছাপূরণের ব্যাপারে এখানে আগতদের বিশ্বাস এতটাই দৃঢ় যে তাদের অনেকের ইচ্ছা ইতিমধ্যেই পূর্ণ হয়েছে। প্রায় প্রতিদিনই এখানে মেলা বসে যেখানে অনেক কিছু পাওয়া যায়।{:}
)
[3] => Array
(
[name] => Chalan Beel
[post_id] => 3052
[post_link] => http://offroadbangladesh.com/bn/places/chalan-beel/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/02/800px-Chalan_Beel_Natore_Bangladesh_52-300x225.jpg
[post_content] =>
Chalan Beel (Bengali: চলনবিল) is a wetland in Bangladesh. It is a large inland depression, marshy in character, with rich flora and fauna. Forty-seven rivers and other waterways flow into the Chalan Beel. As silt builds up in the beel, its size is being reduced.
Chalan Beel is an extensive lowland area in the lower Atrai basin, and spreads across Singra and Gurudaspur upazilas on Natore District, Chatmohar, Bhangura and Faridpur upazilas of Pabna District, and Ullahpara, Raiganj and Tarash upazilas of Sirajganj District. It consists of a series of beels connected to one another by various channels to form a continuous water body during the rainy season. Although the beel area expands into a vast water body with dense aquatic vegetation as long as the Jamuna remains flooded during the monsoon months, it dries out in the winter months, leaving only patches of water in the central parts of this zone.
Chalan Beel is fast silting up. In the past it covered an area of about 1,085 km² but was reduced to 368 km² in 1909, of which only 85 km² remained underwater throughout the year. It has since shrunk to only 26 km².
The most important factor dominating the river history in Bengal is the large proportion of silt carried by its rivers. It is the silt which has created the land and made it habitable by building it up through the centuries. It is silt which is fertilising the land, but the silt, which has been the most beneficial gift of nature, has also produced most of the river problems now confronting the people of Bengal. Silt deposited in the old river channel beds has forced them to change course, creating problems for abandoned areas while assisting in developing new areas.
The main volume of water from the Ganges River began flowing through the Padma channel in the sixteenth century. Silt from the Padma helped in building up the southern portion of north Bengal. This is the most plausible explanation for the existence of a depression around Chalan Beel. The Teesta was active in the region until it changed its course in 1787. This territory lies in between the land raised in the north by the Teesta system when it was active and that in the south by the Padma.
However, there is another explanation for the creation of the depression. The Padma has been changing its course over the centuries. In Ven den Brouck's map of Bengal, prepared in 1660, the main channel of the Padma is shown as flowing through Faridpur-Bakharganj, but there also is a suggestion of another, possibly earlier channel. This channel runs through Rampur Boalia in Rajshahi, Chalan Beel, Dhaleswari and Buriganga before meeting the Meghna. At that time the Jamunawas virtually non-existent and the Brahmaputra used to flow through its old channel.
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