{"description":"\u305d\u308c\u306f\u30d8\u30a4\u30ef\u30fc\u30c9\u65ad\u5c64\u306b\u8d77\u56e0\u3059\u308b\u5730\u9707\u3002\u524d\u56de\u304c\u660e\u6cbb\u7dad\u65b0\u306e\u5e74\u30011868\u5e74\u306e10\u670821\u65e5\u3002\u3067\u3001\u30d8\u30a4\u30ef\u30fc\u30c9\u65ad\u5c64\u306e\u5730\u9707\u306f\u5e73\u5747140\u5e74\u304a\u304d\u306b\u8d77\u304d\u3066\u3044\u308b\u3089\u3057\u3044\u3002 The Bay Area is lined with faults capable of delivering a knock-out blow. But one in particular is poised to rupture sooner than later. Geologists have determined that the average time between major earthquakes on the Hayward f\u2026","version":"1.0","type":"rich","categories":["\u3056\u308c\u3054\u3068"],"image_url":"http://blog.wired.com/wiredscience/images/2008/10/20/shakingintensity.jpg","html":"<iframe src=\"https://hatenablog-parts.com/embed?url=https%3A%2F%2Fnaotoj.hatenablog.com%2Fentry%2F20081021%2F1224647921\" title=\"\u4eca\u65e5\u3067140\u5468\u5e74\u3002 - Hole In The Wall\" class=\"embed-card embed-blogcard\" scrolling=\"no\" frameborder=\"0\" style=\"display: block; width: 100%; height: 190px; max-width: 500px; margin: 10px 0px;\"></iframe>","published":"2008-10-21 12:58:41","blog_url":"https://naotoj.hatenablog.com/","title":"\u4eca\u65e5\u3067140\u5468\u5e74\u3002","provider_url":"https://hatena.blog","author_name":"naotoj","url":"https://naotoj.hatenablog.com/entry/20081021/1224647921","provider_name":"Hatena Blog","width":"100%","author_url":"https://blog.hatena.ne.jp/naotoj/","height":"190","blog_title":"Hole In The Wall"}