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{"type":"standard","title":"Hachisuka Iemasa","displaytitle":"Hachisuka Iemasa","namespace":{"id":0,"text":""},"wikibase_item":"Q1073557","titles":{"canonical":"Hachisuka_Iemasa","normalized":"Hachisuka Iemasa","display":"Hachisuka Iemasa"},"pageid":12874536,"thumbnail":{"source":"https://upload.wikimedia.org/wikipedia/commons/thumb/0/0e/Tokushima_Hachisuka_Iemasa_M3752b.jpg/330px-Tokushima_Hachisuka_Iemasa_M3752b.jpg","width":320,"height":213},"originalimage":{"source":"https://upload.wikimedia.org/wikipedia/commons/0/0e/Tokushima_Hachisuka_Iemasa_M3752b.jpg","width":1500,"height":1000},"lang":"en","dir":"ltr","revision":"1242855738","tid":"553aabd5-65ba-11ef-804a-307a15824440","timestamp":"2024-08-29T03:54:04Z","description":"Japanese daimyō","description_source":"local","content_urls":{"desktop":{"page":"https://en.wikipedia.org/wiki/Hachisuka_Iemasa","revisions":"https://en.wikipedia.org/wiki/Hachisuka_Iemasa?action=history","edit":"https://en.wikipedia.org/wiki/Hachisuka_Iemasa?action=edit","talk":"https://en.wikipedia.org/wiki/Talk:Hachisuka_Iemasa"},"mobile":{"page":"https://en.m.wikipedia.org/wiki/Hachisuka_Iemasa","revisions":"https://en.m.wikipedia.org/wiki/Special:History/Hachisuka_Iemasa","edit":"https://en.m.wikipedia.org/wiki/Hachisuka_Iemasa?action=edit","talk":"https://en.m.wikipedia.org/wiki/Talk:Hachisuka_Iemasa"}},"extract":"Hachisuka Iemasa was a Japanese daimyō of the early Edo period. Iemasa, the son of Hachisuka Masakatsu or Koroku, was the founder of the Tokushima Domain. He was one of some daimyo who have bad terms with Ishida Mitsunari.","extract_html":"
Hachisuka Iemasa was a Japanese daimyō of the early Edo period. Iemasa, the son of Hachisuka Masakatsu or Koroku, was the founder of the Tokushima Domain. He was one of some daimyo who have bad terms with Ishida Mitsunari.
"}{"type":"standard","title":"Geology of Socotra","displaytitle":"Geology of Socotra","namespace":{"id":0,"text":""},"wikibase_item":"Q55612489","titles":{"canonical":"Geology_of_Socotra","normalized":"Geology of Socotra","display":"Geology of Socotra"},"pageid":57697542,"thumbnail":{"source":"https://upload.wikimedia.org/wikipedia/commons/thumb/2/25/Socotra_Geology.jpg/330px-Socotra_Geology.jpg","width":320,"height":206},"originalimage":{"source":"https://upload.wikimedia.org/wikipedia/commons/2/25/Socotra_Geology.jpg","width":1024,"height":659},"lang":"en","dir":"ltr","revision":"1275533223","tid":"3e7fe5f5-ea26-11ef-8ea0-fa00085e5e57","timestamp":"2025-02-13T16:19:05Z","description":"Regional geology of part of Yemen","description_source":"local","content_urls":{"desktop":{"page":"https://en.wikipedia.org/wiki/Geology_of_Socotra","revisions":"https://en.wikipedia.org/wiki/Geology_of_Socotra?action=history","edit":"https://en.wikipedia.org/wiki/Geology_of_Socotra?action=edit","talk":"https://en.wikipedia.org/wiki/Talk:Geology_of_Socotra"},"mobile":{"page":"https://en.m.wikipedia.org/wiki/Geology_of_Socotra","revisions":"https://en.m.wikipedia.org/wiki/Special:History/Geology_of_Socotra","edit":"https://en.m.wikipedia.org/wiki/Geology_of_Socotra?action=edit","talk":"https://en.m.wikipedia.org/wiki/Talk:Geology_of_Socotra"}},"extract":"The geology of Socotra is part of the national geology of Yemen. Ancient Precambrian metamorphic rocks are intruded by younger igneous rocks, overlain by limestones and other marine sediments that deposited during marine transgression periods in the Cretaceous and the past 66 million years of the Cenozoic. The island is on the Somali Plate, which rifted away from the Arabian mainland within the past 60 million years.","extract_html":"
The geology of Socotra is part of the national geology of Yemen. Ancient Precambrian metamorphic rocks are intruded by younger igneous rocks, overlain by limestones and other marine sediments that deposited during marine transgression periods in the Cretaceous and the past 66 million years of the Cenozoic. The island is on the Somali Plate, which rifted away from the Arabian mainland within the past 60 million years.
"}