{"type":"standard","title":"Bagerhat","displaytitle":"Bagerhat","namespace":{"id":0,"text":""},"wikibase_item":"Q13058909","titles":{"canonical":"Bagerhat","normalized":"Bagerhat","display":"Bagerhat"},"pageid":2241765,"thumbnail":{"source":"https://upload.wikimedia.org/wikipedia/commons/thumb/f/f3/Bagerhat_Central_Shahid_Minar.jpg/330px-Bagerhat_Central_Shahid_Minar.jpg","width":320,"height":213},"originalimage":{"source":"https://upload.wikimedia.org/wikipedia/commons/f/f3/Bagerhat_Central_Shahid_Minar.jpg","width":3948,"height":2632},"lang":"en","dir":"ltr","revision":"1269767324","tid":"e6cb6e16-d3e0-11ef-8b4c-d7beff87de46","timestamp":"2025-01-16T08:07:17Z","description":"City & Municipality in Khulna, Bangladesh","description_source":"local","coordinates":{"lat":22.653,"lon":89.792},"content_urls":{"desktop":{"page":"https://en.wikipedia.org/wiki/Bagerhat","revisions":"https://en.wikipedia.org/wiki/Bagerhat?action=history","edit":"https://en.wikipedia.org/wiki/Bagerhat?action=edit","talk":"https://en.wikipedia.org/wiki/Talk:Bagerhat"},"mobile":{"page":"https://en.m.wikipedia.org/wiki/Bagerhat","revisions":"https://en.m.wikipedia.org/wiki/Special:History/Bagerhat","edit":"https://en.m.wikipedia.org/wiki/Bagerhat?action=edit","talk":"https://en.m.wikipedia.org/wiki/Talk:Bagerhat"}},"extract":"Bagerhat is a city in southern Bangladesh and the headquarters of Bagerhat district. Located on the banks of the Bhairab river, Bagerhat has a population of around 50,000. It is located near the old city of Khalifatabad, now a UNESCO World Heritage Site.","extract_html":"
Bagerhat is a city in southern Bangladesh and the headquarters of Bagerhat district. Located on the banks of the Bhairab river, Bagerhat has a population of around 50,000. It is located near the old city of Khalifatabad, now a UNESCO World Heritage Site.
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{"slip": { "id": 34, "advice": "To improve productivity, always have a shittier task to put off."}}
{"fact":"A cat has two vocal chords, and can make over 100 sounds.","length":57}
{"slip": { "id": 90, "advice": "Brush your teeth the moment you get up."}}
{"type":"standard","title":"Lake Hitchcock","displaytitle":"Lake Hitchcock","namespace":{"id":0,"text":""},"wikibase_item":"Q3214929","titles":{"canonical":"Lake_Hitchcock","normalized":"Lake Hitchcock","display":"Lake Hitchcock"},"pageid":1756307,"thumbnail":{"source":"https://upload.wikimedia.org/wikipedia/commons/thumb/f/f4/Glacial_Lakes_Albany%2C_Champlain%2C_Hitchcock%2C_Winsooski%2C_%26_Merrimack.jpg/330px-Glacial_Lakes_Albany%2C_Champlain%2C_Hitchcock%2C_Winsooski%2C_%26_Merrimack.jpg","width":320,"height":414},"originalimage":{"source":"https://upload.wikimedia.org/wikipedia/commons/f/f4/Glacial_Lakes_Albany%2C_Champlain%2C_Hitchcock%2C_Winsooski%2C_%26_Merrimack.jpg","width":918,"height":1188},"lang":"en","dir":"ltr","revision":"1286753903","tid":"33937f0a-1ee9-11f0-b1e8-13bd18100a6a","timestamp":"2025-04-21T19:45:39Z","description":"Former glacially-formed lake of New England","description_source":"local","coordinates":{"lat":41.81666667,"lon":-72.63333333},"content_urls":{"desktop":{"page":"https://en.wikipedia.org/wiki/Lake_Hitchcock","revisions":"https://en.wikipedia.org/wiki/Lake_Hitchcock?action=history","edit":"https://en.wikipedia.org/wiki/Lake_Hitchcock?action=edit","talk":"https://en.wikipedia.org/wiki/Talk:Lake_Hitchcock"},"mobile":{"page":"https://en.m.wikipedia.org/wiki/Lake_Hitchcock","revisions":"https://en.m.wikipedia.org/wiki/Special:History/Lake_Hitchcock","edit":"https://en.m.wikipedia.org/wiki/Lake_Hitchcock?action=edit","talk":"https://en.m.wikipedia.org/wiki/Talk:Lake_Hitchcock"}},"extract":"Lake Hitchcock was a glacial lake that formed approximately 15,000 years ago in the late Pleistocene epoch. After the Laurentide Ice Sheet retreated, glacial ice melt accumulated at the terminal moraine and blocked up the Connecticut River, creating the long, narrow lake. The lake existed for approximately 3,000 years, after which a combination of erosion and continuing geological changes likely caused it to drain. At its longest, Lake Hitchcock stretched from the moraine dam, at present-day Rocky Hill, Connecticut, north to St. Johnsbury, Vermont. Although the rift valley through which the river flows above Rocky Hill actually continues south to New Haven, on Long Island Sound, the obstructing moraine at Rocky Hill diverted the river southeast to its present mouth at Old Saybrook.","extract_html":"
Lake Hitchcock was a glacial lake that formed approximately 15,000 years ago in the late Pleistocene epoch. After the Laurentide Ice Sheet retreated, glacial ice melt accumulated at the terminal moraine and blocked up the Connecticut River, creating the long, narrow lake. The lake existed for approximately 3,000 years, after which a combination of erosion and continuing geological changes likely caused it to drain. At its longest, Lake Hitchcock stretched from the moraine dam, at present-day Rocky Hill, Connecticut, north to St. Johnsbury, Vermont. Although the rift valley through which the river flows above Rocky Hill actually continues south to New Haven, on Long Island Sound, the obstructing moraine at Rocky Hill diverted the river southeast to its present mouth at Old Saybrook.
"}