Where to Stay
There are many hotels available in Chittagong. Some of them have been mentioned below for your help.
1. Hotel Golden Inn
Address: 336 Station Rd Chittagong
Contact: 611 004
2. Asian SR Hotel
Address: 291 Station Rd Chittagong
Contact: 031-2850346-8, 01711-889555
3. Hotel Park
Address: 627, DT road, Kadamtoli Chittagong
Contact: 01819-388011
4. Hotel Landmark
Address: 3072, Sheikh Mujhibar Road, Agrabad, Chittagong
Contact: 031-813598/727299
5. Hotel Dream International Ltd
Station Road, Chittagong, Bangladesh
01829-440044
6. Hotel Azad
Enayet Bazar, Chittagong, Bangladesh
7. Hotel Mishka
Station Road, Chittagong 4000, Bangladesh
8. Motel Shaikat
Station Road, Chittagong, Bangladesh
Array
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[0] => Array
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[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।{:}
)
[1] => 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.
)
[2] => Array
(
[name] => Balia Dighi
[post_id] => 3609
[post_link] => http://offroadbangladesh.com/places/balia-dighi/
[thumb_link] => http://offroadbangladesh.com/wp-content/uploads/2015/02/Balia-Dighi-300x225.jpg
[post_content] => Raja Ballal Sen excavated the Balia Dighi. Many say that since it is a sandy dighi so it is known as Balia Dighi. It is located on south of Kotowali gate. Its volume is 39.8 acre.
)
[3] => Array
(
[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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