Array
(
[0] => Array
(
[name] => {:en}Bisanakandi{:}{:bn}বিছানাকান্দি{:}
[post_id] => 7828
[post_link] => http://offroadbangladesh.com/bn/places/bisanakandi/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/04/10410793_10205865808218505_7613722895639363442_n-300x188.jpg
[post_content] => {:en}
Bisanakandi is situated at Bangladesh-India border in Sylhet. It is a landscape beauty among gardens and hills. Bichanakandi is a village situated in Rustompur Union under Guainghat Upazilla. This is where many layers of the Khasi mountain meet at a single point from both sides. Flowing from above is a high fall. Adding to its charm are dark clouds hugging the mountain in the rainy season. And flowing underneath towards Bholaganj is a branch of the Piyain. Along the stream flowing from high up in the mountain come huge boulders that are deposited and mined in Bisanakandi.
Much like Jaflong, Bichnakandi is mostly a quarry. Winter is not a suitable time to visit Bisnakandi due to mechanized mining and stone-laden boats and lorries. The absence of such nuisance makes the rainy season the perfect time to visit the beautiful Bisanakandi that coalesces the charms of high mountains, sinuous rivers, graceful falls and dancing clouds.
Source:
Visit Sylhet{:}{:bn}
সিলেটের গোয়াইনঘাট উপজেলার রুস্তম ইউনিয়নে বাংলাদেশ-ভারত সীমান্তে অবস্থিত একটি গ্রামের নাম বিছানাকান্দি। বাগান এবং পাহাড়ের নজরকাড়া সৌন্দর্যের মাঝে অবস্থিত প্রকৃতির এই অপরূপ লীলাভূমির উভয় প্রান্ত থেকে খাসি পাহাড় এসে যুক্ত হয়েছে। এখানে ঝর্ণার পাশাপাশি বর্ষাকালে কালো মেঘ পাহাড়গুলোকে আচ্ছাদিত করে ফেলে। এছাড়া এখানে ভোলাগঞ্জ অভিমুখে বয়ে গিয়েছে পিইয়াইন নদীর একটি শাখা। পাহাড়ি ঢলের সাথে বয়ে আসা বিশাল পাথরখণ্ডগুলো বিছানাকান্দিতে এসে পড়ে এবং পরবর্তীতে এই পাথরখণ্ডগুলোকে এখানেই ভাঙ্গা হয়।
জাফলং এর মত বিছানাকান্দিও একটি খনি এলাকা। পাথর বোঝাই নৌকা, ট্রাকের আনাগোনা এবং পাথর উত্তোলনের কারনে শীতকাল বিছানাকান্দিতে আসার জন্য একেবারেই উপযুক্ত সময় নয়। তবে, বর্ষাকালে এখানে পাথর উত্তোলনের ফলে সৃষ্ট দূষণ না থাকায় আপনি এখানে এসে উঁচু পাহাড়, শান্ত নদী, মায়াবি ঝর্ণার সৌন্দর্যের পাশাপাশি রোদ ও মেঘের লুকোচুরি উপভোগ করতে পারবেন।
{:}
)
[1] => Array
(
[name] => Karotoya River
[post_id] => 1149
[post_link] => http://offroadbangladesh.com/bn/places/karotoya-nodi/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/01/BD_Korotoa_River-300x225.jpg
[post_content] =>
Karatoya River (also spelt Korotoa) (Bengali:
করতোয়া নদী), a small stream in Rajshahi Division of Bangladesh, was once a large and sacred river. A channel of it presently flows by the ancient ruins of Mahasthangarh (or Pundranagara, ancient capital of Pundravardhana) in Bogra District. The
Karatoya mahatmya bears testimony to its past greatness. In the
Mahabharata it is mentioned that a visit to the Karatoya after three days’ fast produces the same merit as an aswamedha (horse killing) sacrifice. Another ancient city, Sravasti, may have been located on the banks of the Karatoya, north of Mahasthangarh. However, there is a controversy about the possible location of Sravasti.
The Karatoya, known as Phuljhur rises in the Baikunthapur jungles in the extreme north-west of Jalpaiguri district (West Bengal, India) and forms for some distance the boundary between Dinajpur and Rangpur districts. It, then, meanders through Rangpur and Bogra. In the south of Bogra district, it receives the Halhalia and the united stream is then known as Phuljhur. It leaves Bogra at Chanda kona and flowing in a southerly direction past Raiganj and Shujapur is, as already mentioned, joined by lchhamati at Nalka. The Phuljhur then flows south past the important village of Ullapara, a few miles below which it joins the Hurasagar at Narnia after a course of about 64 kilometres (40 mi) in this district. After this junction, it takes the name of Hurasagar and passing close by Shazadpur and Hera joins the Jamuna near Bera.
The Karatoya is mentioned in the Puranas and had a high repute for sanctity. It was the eastern boundary of the old kingdom of Paundravardhana, the country of the Paundras which it separated from Kamrupa. It is shown in Van Den Brouk's map of Bengal (C, 1660) as flowing into the Ganges and in fact. before the destructive floods of 1787 it brought down to the Atrai and to the Ganges a great volume of Teesta water. Since the main stream of the Teesta was dirverted to the east in 1787, the Karatoya and the Phuljhur have gradually silted up. and they are at the present day rivers of minor importance. One channel, which joins the Baral, 48 kilometres (30 mi) east of Pabna. is still called indifferently the Buri Teesta or old Teesta and the Karto or Karatoya. Traces of an old channel, for which the name of the Karatoya is claimed, are also pointed out in the Chatmohar thana, where it appears to have been obliterated by the Baral.
)
[2] => Array
(
[name] => {:en}Sangu River{:}{:bn}সাঙ্গু নদী{:}
[post_id] => 5349
[post_link] => http://offroadbangladesh.com/bn/places/sangu-river/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/03/2Sangu-river1-300x200.jpg
[post_content] => {:en}
The Sangu River is a river in Myanmar and Bangladesh. Its source is in the North Arakan Hills of Myanmar, located at 21°13´N 92°37´E. The Arakan Hills form the boundary between Arakan and the Chittagong Hill Tracts. It follows a northerly circuitous course in the hill tracts and then enters Bangladesh near Remarki, Thanchi Upazila, Bandarban District, from the east. It flows north through Thanchi, Rowangchhari and Bandarban Sadar Upazilas of Bandarban District. It then flows west through Satkania and Banshkhali Upazilas in Chittagong District and flows into the Bay of Bengal near Chittagong, at 22°6´N 91°51´E, or about 16.09 kilometres (10.00 mi) south of the mouth of the Karnafuli River. The length of the river is 270 kilometres (170 mi); 173 kilometres (107 mi) are located within Bangladesh.
Sangu River is the complete part of the natural beauty of Bandarban. It follows a northerly circuitous course in the hill tracts up to Bandarban. It enters the district from the east and flows west across the district and finally falls into the Bay of Bengal at the end of a course of 270 km. This river is flowing through the hills thousands of years. It is an important route to communicate with Ruma and Thanchi Upazila. It has huge financial interests for the population of Bandarban. This river is widely used for transportation, agricultural and other necessary products for the people of remote community.
In the winter season the current of the river almost becomes stagnant but in the rainy season the current becomes aggressive. Visitor must be attract with the beautification scattered on the both sides of it. You can find here hills, forests, falls with a river together. All the way you will be thrilled only and it is simply amazing.
The major tributaries of the river are the Chand Khali Nadi and Dolukhal. The Chand Khali Nadi flows through the Patiya Plains, and the Dolukhal River drains into the Satkania Plains. Another tributary is the Kumira Khali, which drains into the Kutubdia Channel. There are seven Bangladesh Water Management Board hydrometric stations on this river, which have been recording data since 1965.
The Sangu drains off the waters of Patiya, Satkania, and Banshkhali Upazilas. It has a connection with the Karnafuli River through the Chand Khali River. The Sangu is a shallow river, but it becomes violent during rains and develops rapid currents. It is navigable up to 48.27 kilometres (29.99 mi) from the estuary. The Sangu gas field is located about 50 kilometres (31 mi) southwest of Chittagong and reaches a depth of 10 meters at its mouth.
{:}{:bn}
বান্দরবানের প্রাকৃতিক সৌন্দর্যের অন্যতম অংশ সাঙ্গু নদী পার্বত্য চট্রগ্রামে উত্তরদিকে বৃত্তাকারে বান্দরবান পর্যন্ত প্রবাহিত হয়েছে। পূর্বদিক দিয়ে বান্দরবানে প্রবেশ করে নদীটি জেলার পশ্চিম দিক দিয়ে বের হয়েছে এবং প্রায় ২৭০ কিলোমিটার প্রবাহিত হওয়ার পর বঙ্গোপসাগরে মিলিত হয়েছে। পার্বত্য অঞ্চলে হাজার বছর ধরে প্রবাহিত এই নদীটি রুমা এবং থানচি উপজেলার সাথে যোগাযোগের এক গুরুত্বপূর্ণ মাধ্যম। বান্দরবানের জনগনের অর্থনৈতিক প্রবৃদ্ধিতে এই নদীটি গুরুত্বপূর্ণ ভুমিকা পালন করছে। দুর্গম এই অঞ্চলের মানুষেরা পরিবহন, কৃষি এবং অন্যান্য প্রয়োজনীয় কাজে নদীটিকে বহুভাবে ব্যবহার করে থাকে।
শীতকালে সাঙ্গুনদীর স্রোত অনেকাংশে ম্রিয়মাণ হয়ে গেলেও বর্ষাকালে নদীটির স্রোত তীব্র আকার ধারন করে। সাঙ্গু নদীর দুই তীরের পাহাড়, বন, নদী ও ঝর্ণার সৌন্দর্যে যেকোনো পর্যটকই বিমোহিত হবেন। এক কথায় সাঙ্গুনদী দেখে আপনি শুধু অবাকই হবেন না বরং মুগ্ধতা আপনাকে গ্রাস করবে।
{:}
)
[3] => Array
(
[name] => Buriganga River
[post_id] => 7432
[post_link] => http://offroadbangladesh.com/bn/places/buriganga-river/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/04/Buriganga-River21-300x240.jpg
[post_content] =>
The Buriganga River (বুড়িগঙ্গা), previously known as "Old Ganges", flows past the southwest outskirts of Dhaka city, the capital of Bangladesh. Its average depth is 7.6 meters (25 ft.) and its maximum depth is 18 meters (58 ft.). In the distant past, a course of the Ganges River used to reach the Bay of Bengal through the Dhaleswari River.
When this course gradually shifted and ultimately lost its link with the main channel of the Ganges it was renamed the Buriganga. It is said that the water levels during high and very high tides in this river astonished the Mughals. In the 20th century the water table and river became polluted by polythene and other hazardous substances from demolished buildings near the river banks.
Photograph of Dacca (Dhaka) taken in the 1880s, from an album 'Architectural Views of Dacca', containing 13 prints by Johnston and Hoffman. View looking along the river Buriganga towards the city of Dhaka situated on the left bank. A Hindu temple tower stands at the water's edge.
)
)
