Array
(
[0] => Array
(
[name] => {:en}Jaflong{:}{:bn}জাফলং{:}
[post_id] => 4142
[post_link] => http://offroadbangladesh.com/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] => {:en}Limestone Lake of Tekerghat{:}{:bn}টেকেরঘাট চুনাপাথরের লেক{:}
[post_id] => 9066
[post_link] => http://offroadbangladesh.com/places/limestone-lake-of-tekerghat/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/05/Limestone-Lake-of-Tekerghat1-300x225.jpg
[post_content] => {:en}
Limestone Lake of Tekerghat is located near the Tanguar Haor, so close to Indian border. Once upon a time there was a limestone quarry, but now-a-days that one is not functioning. The Tekerghat Limestone Lake (টেকেরঘাট চুনাপাথরের লেক) is minimum 18 kilometers north from the Tahirpur town.
The water of the lake is clear. You might the water of the lake would be blue. But still the water isn’t bad. This lake was created by quarrying the limestone. Exactly other side of the lake is India. People from India usually take their bath at that side. Hill of that side has large boulders of limestone, but all belongs to India.
There are few small Tila (টিলা) available in Bangladesh side, possibly 20 ft. height and artificial. You can pass few minutes on those if you like.
{:}{:bn}টাঙ্গুয়ার হাওড়ের কাছে ভারত সীমান্তবর্তী একটি স্থানের নাম টেকেরঘাট। একসময় এখানে একটি চুনাপাথরের খনি থাকলেও বর্তমানে খনিটির কার্যকারিতা আর নেই। তাহিরপুর থেকে অন্তত ১৮ কিলোমিটার উত্তরে টেকেরঘাট চুনাপাথরের লেক অবস্থিত।
টেকেরঘাট চুনাপাথরের লেকের পানি নীল না হলেও বেশ পরিষ্কার। চুনাপাথর খননের ফলে এই লেকটির সৃষ্টি হয়। টেকেরঘাট চুনাপাথরের লেকের অপর প্রান্তে ভারত অবস্থিত হওয়ায় সেখানকার অধিবাসীরা লেকে গোসল করে থাকে। লেকের ভারতীয় অংশের পাহাড়ে চুনা পাথরের বিশাল খণ্ড রয়েছে।
টেকেরঘাট চুনাপাথরের লেকের বাংলাদেশ প্রান্তে প্রায় ২০ ফুট উচ্চতার কয়েকটি কৃত্রিম ছোট টিলা রয়েছে। আপনি চাইলে এসব টিলার উপর উঠে কিছু সময় কাটাতে পারেন।{:}
)
[2] => Array
(
[name] => Rampal Dighi
[post_id] => 8867
[post_link] => http://offroadbangladesh.com/places/rampal-dighi/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/05/rampal-21-300x169.jpg
[post_content] => Rampal Dighi is one of the most ancient Dighi(large pond) in Munshiganj District. It is about 1500m long from north to south and 300m wide. Recently built Rampal College stands on its northern bank. Rampal Dighi covers an area of about 55 acres of land.
The Lake of Legend:
Ballal Sen (Bengali: বল্লাল সেন; reign: 1160–1179) was the second ruler of the Sen dynasty of Bengal. He was the son and successor of Vijay Sen, the founder of Sen dynasty. King Bollal Sen was a famous ruler of Sen dynasty in Bikrompur. One day his mother told him that the tenants need a good & suitable source of water for their everyday use. The kind King set arrangement for making a very large pond. Actually his mother was instructed by some Angelic figures in a lucid dream. So,according to her dream she decided to walk a mile. Her walkway will be the area of the pond. After the pond is being dug, there was no water at all. Again according to the instruction of an angelic entity the King decided to sacrifice himself. But at last moment kings friend Rampal took his place. Rampal sacrificed himself and the pond was filled with water instantly. But unfortunately today there is no water in this pond anymore.
)
[3] => Array
(
[name] => Chalan Beel
[post_id] => 3052
[post_link] => http://offroadbangladesh.com/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.
)
)
