Brief
The blue water lake of Birisiri (বিরিশিরি) is located at the Kulagora Upazila (কুলাগরা উপজেলা) of Durgapur Thana (দুর্গাপুর থানা) from Netrakona district (নেত্রকোনা জেলা). People call this lake as China Matir Lake, China Clay Lake (চিনা মাটির লেক), Limestone Lake, Neel Pukur (নীল পুকুর), etc. Main attraction of the lake is the water which having blue color in winter.
This is a small lake, you can say this is a pond as well. Normally the water from a pond used to be muddy, or greenish during winter. But this one is having blue color just because the china clay. This blue pond is generated after digging out china clay. According to the local people, the depth of the small pond is somewhere around 60-80 feet.
China clay comprises of lot of chemical compounds. The taste of the water is kind of bitter. May be the lake water has plenty of copper sulphet which can make the water color blue.
During your way to the blue lake, you’ll be enthralled by the picturesque view of the village and the beautiful shomeswari river (সমেস্বারী নদী). The ride was so exciting that anyone would love to do that again.
If you are a good swimmer, and confident enough over your ability, you can bring shorts to cool your body from the lake. I am sorry but there is no space for non-swimmer to take chance.
Possibly this is the only clay lake having blue water from Bangladesh (বাংলাদেশ). Mymensingh (ময়মনসিংহ) has one, but that one is not that much beautiful like this one. So don’t make the place messy by dropping your crumbs around (or inside) the lake.
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[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.
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[name] => Sindurmoti Dighi
[post_id] => 4751
[post_link] => http://offroadbangladesh.com/places/sindurmoti-dighi/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/02/offroadbangladeshlogo2-300x178.png
[post_content] =>
It is situated at Panchagram in Lanlmonirhat district. In the month of Chaitra the peoples of hindus do worship. People says that A Hindu landowner Narayan Chakrawarti dag this pond cause of draught. But cause of having no water in the pond he got a dream to worship by leaving two daughter of him in the middle of the pond named Sindur and Mati. But he failed to bring all the elements for the worship. When he went to take all the elements the pond fulfilled with water. The two daughter of the lanowner failed to reach in the bank and died. After that he saw a dream that his two daughter got immortality.
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[name] => Shukhbashpur Dighi
[post_id] => 8933
[post_link] => http://offroadbangladesh.com/places/shukhbashpur-dighi/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/07/Sukhobashpur-1-300x169.jpg
[post_content] => Shukhbashpur Dighi (সুখবাসপুর দিঘী), nearly hundred years old Lake situated at Hatimara, Rampal Union Parishad of Munshiganj Sadar. Almost all around the year it is filled with water. It is a rectangular shaped lake which is surrounded by different types of green trees. Its natural beauty, gentle breeze, calm and quiet environment attracts people to spend their leisure time at the edge of this dighi. Above all, its oldness and different types of myth also make people visit this place.
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[name] => {:en}Hakaluki Haor{:}{:bn}হাকালুকি হাওড়{:}
[post_id] => 6360
[post_link] => http://offroadbangladesh.com/places/hakaluki-haor/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/04/Hakaluki-Haor1-300x225.jpg
[post_content] => {:en}
Hakaluki Haor is a marsh wetland ecological system of Eastern Bangladesh in an area bordering Assam, India. It is one of Bangladesh's largest and one of Asia's larger marsh wetland resources. Some 190,000 people live in the surrounding Hakaluki Haor area.
Hakaluki Haor was designated an Ecologically Critical Area (ECA). It’s also a protected Ramsar site of international importance for the conservation and sustainable utilization of wetlands.
The surface area of Hakaluki Haor is 181.15 km2, of which 72.46 km2 (40.01%) is within the territory of Barlekha Upazila. The Haor is partly under the jurisdiction of Barlekha Upazila.
[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}হাকালুকি হাওড় মূলত মৌলভীবাজার জেলার বড়লেখা উপজেলায় অবস্থিত। ভারতের আসাম সীমান্তবর্তী বাংলাদেশের পূর্ব অংশে অবস্থিত একটি জলাভূমি হল হাকালুকি হাওড়। এটি বাংলাদেশের বৃহত্তম এবং এশিয়ার অন্যতম বৃহৎ জলাভূমি। পরিবেশগত গুরুত্বপূর্ণ এলাকা (ইসিএ) হিসেবে ঘোষিত এই হাওড়ের আশেপাশে প্রায় ১,৯০,০০০ মানুষ বসবাস করেন। জলাভুমির যথাযথ ব্যবহার এবং সংরক্ষণের ওপর গুরুত্বের কারনে এই জলাভূমিটির সুরক্ষার ওপর আন্তর্জাতিকভাবে মনোনিবেশ করা হয়েছে। ১৮১.১৫ কিলোমিটার আয়তনের এই জলাভূমিটির প্রায় ৭২.৪৬ কিলোমিটার অর্থাৎ ৪০.০১% ভাগ বড়লেখা উপজেলায় অবস্থিত।{:}
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