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| "nt":"降雨过后发生的滑坡，滑坡特征明显，醉汉林可视，滑坡后壁较大。",
| "tm":"2017-12-13 06:47:12",
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| "nt":"2010年7月27日汉源县万工乡双合村一组万工集镇后背山（小地名二蛮山）发生山体滑坡，滑坡现场斜坡长1.6公里，高度620米，垮塌土石方量约120万立方米。造成万工集镇、双合一组部分村民房屋垮塌，部分房屋被掩埋。截至7月27日14时25分，灾害已造成20人失踪，91户（涉及391人）房屋倒塌。414户1338人房屋受到影响。",
| "tm":"2017-11-28 17:14:38",
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| "location":"四川-汉源",
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| "nt":"海城地震是1975年2月4日发生于今天中国辽宁省海城市的大地震。1975年2月4日北京时间19点36分，在辽宁省海城、营口县一带（东经122°50'，北纬40°41'）发生了强度是里氏7.3级（矩震级7.0级）的强烈地震，震源深度为16－21公里。由于中国科学家对该次地震进行了准确预测并及时发布了短临预报，全区人员伤亡共18308人，仅占总人口数的0.22%。其中，死亡1328人，占总人口数的0.02%，重伤4292人，轻伤12688人，轻重伤占总人口数的0.2%。部分人认为，这是人类历史上迄今为止，在正确预测地震的基础上，由官方组织撤离民众，明显降低损失的唯一成功案例。",
| "tm":"2017-11-20 13:10:57",
| "lineid":null,
| "geo_yanxing":null,
| "location":"辽宁-海城",
| "type":"2",
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| "creator":"henry",
| "id":"79e8071f50994e5382c39c309df02e14",
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| "name":"1975年海城7.3级地震",
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| "nt":"1970年1月5日凌晨，云南通海、峨山、建水等地，发生了死亡人数超过一万五千人的7.8级大地震。震源深度仅134米，主震后发生5级至5.9级余震12次，引起严重滑坡、山崩等破坏，受灾面积4500多平方公里，造成15621人死亡，338456间房屋倒塌，166338头大牲畜死亡，生命财产损失巨大。",
| "tm":"2017-11-20 13:07:37",
| "lineid":null,
| "geo_yanxing":null,
| "location":"云南通海",
| "type":"2",
| "is_use":1,
| "lttd":24.06,
| "creator":"henry",
| "id":"f190d89886d144a2af13dd84dfb9f2fb",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"1970年通海7.8级地震",
| "disaster_geo_yanxing":"1",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"6",
| "videos":"",
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| "country":null,
| "lgtd":102.35,
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| {
| "nt":"邢台地震由两个大地震组成：1966年3月8日5时29分14秒，河北省邢台专区隆尧县（北纬37度21分，东经114度55分）发生震级为6.8级的大地震，震中烈度9度强；1966年3月22日16时19分46秒，河北省邢台专区宁晋县（北纬37度32分，东经115度03分）发生震级为7.2级的大地震，震中烈度10度。两次地震共死亡8064人，伤38000人，经济损失10亿元。这是一次久旱之后的大震。地震发生后，漫天飘雪。中国总理周恩来三赴震区，百姓的苦难使他落泪，他指示中国一定要有自己的地震预报系统。中国的地震预报事业在邢台地震的血泊中矗立起划时代的里程碑。",
| "tm":"2017-11-20 13:04:48",
| "lineid":null,
| "geo_yanxing":null,
| "location":"河北-邢台",
| "type":"2",
| "is_use":1,
| "lttd":37.35,
| "creator":"henry",
| "id":"82e71c712ed542d3855e55523c86165f",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"1966年邢台6.8级地震",
| "disaster_geo_yanxing":"1",
| "engineering_type":null,
| "openid":"",
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| "disaster_type":"6",
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| "lgtd":114.916667,
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| "adcd":null,
| "decider":"henry",
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| {
| "nt":"5·12四川汶川特大地震是公元2008年5月12日14时28分04秒（星期一，农历戊子鼠年四月大初八日）发生的8.0级（最大震级14.0级）地震，震中位于四川省汶川县映秀镇与漩口镇交界处（渔子溪长城（中国长城世界遗产）正西方向2.5公里处，牛眠沟莲花心山脚下），东经103°42'，北纬31°01'（美国地质调查局则认可汶川地震发生地点为北纬30.986゜026.25′214.3162″，东经103.364゜276.60′333.0260″）。5·12汶川地震严重破坏地区超过10万平方千米，其中，极重灾区共10个县（市），较重灾区共41个县（市），一般灾区共186个县（市）。截至2008年9月18日12时，5·12汶川地震共造成69227人死亡，374643人受伤，17923人失踪，是中华人民共和国成立以来破坏力最大的地震，也是唐山大地震后伤亡最严重的一次地震。",
| "tm":"2017-11-19 16:27:47",
| "lineid":null,
| "geo_yanxing":null,
| "location":"四川-汶川",
| "type":"2",
| "is_use":1,
| "lttd":31.01,
| "creator":"henry",
| "id":"bf6083cf841e445490b953c5c8cb2df2",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"2008年汶川8.0级地震 ",
| "disaster_geo_yanxing":"1",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"6",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":103.42,
| "archaeology_type":null,
| "images":"GeologicalDisaster/ababdd1f15d648bbbaf2188377db8b06.jpg,GeologicalDisaster/2734938027d5451a9c952414059f7bc4.jpg,GeologicalDisaster/3f6324c5211044eab280fad5b35c4f23.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
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| {
| "nt":"2017年11月13日2时18分在伊朗与伊拉克交界处发生7.8级地震，震源深度20千米。地震在伊朗边境省份克尔曼沙赫造成61人死亡，300多人受伤。",
| "tm":"2017-11-19 16:23:22",
| "lineid":null,
| "geo_yanxing":null,
| "location":"伊朗与伊拉克交界",
| "type":"2",
| "is_use":1,
| "lttd":34.9,
| "creator":"henry",
| "id":"c95594e35f5b4f2395c76df17ccb2d0a",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"2017年伊朗7.8级地震",
| "disaster_geo_yanxing":"1",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"6",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":45.75,
| "archaeology_type":null,
| "images":"GeologicalDisaster/03a5faf064a84457b9ac897eb75220dc.jpg,GeologicalDisaster/77cf6b7dfa1b481f84b5e703d95787e3.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
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| {
| "nt":"2017年11月18日6时34分，在西藏林芝市米林县（北纬29．75度，东经95．02度）发生6．9级地震，震源深度约10公里。截至18日18时，震区共记录到地震总数304次（余震总数303次）。其中5．0至5．9级地震1次，4．0至4．9级地震2次。",
| "tm":"2017-11-19 16:13:14",
| "lineid":null,
| "geo_yanxing":null,
| "location":"西藏-米林",
| "type":"2",
| "is_use":1,
| "lttd":29.75,
| "creator":"henry",
| "id":"00ba12cb2162478fa6b7b3f0299eef50",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"2017年米林6.9级地震 ",
| "disaster_geo_yanxing":"1",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"6",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":95.02,
| "archaeology_type":null,
| "images":"GeologicalDisaster/24f004460b8147f8b6e74c6b8c69508f.jpg",
| "adcd":null,
| "decider":"henry",
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| "nt":"1960年5月21日下午3时，智利发生9.5级大地震。从这一天到5月30日，该国连续遭受数次地震袭击，地震期间，6座死火山重新喷发，3座新火山出现。5月21日的9.5级大地震造成了20世纪最大的一次海啸。这是有仪器记录以来最大的一次地震。地震造成智利2万人死亡。几天之后，地震的能量穿过太平洋，在太平洋西岸掀起了海啸，又给日本和菲律宾的东部沿海地区造成了严重的损害。与此同时，这次地震还引起了巨大的海啸，智利沿海建筑物大部分被海浪卷走，破坏房屋16万栋。此外，海浪还以每小时600公里 ～700公里的速度扫过太平洋，使日本沿海1千多所住宅被冲走，2万多亩良田被淹没。地震激发的海啸也是罕见的，15小时后海啸的大潮波传到夏威夷群岛，22小时后传到日本东海岸，造成巨大损失。这次海啸在日本造成800人死亡，15万人无家可归。",
| "tm":"2017-09-20 17:23:51",
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| "location":"智利",
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| "nt":"1985年9月19日清晨7时19分，墨西哥西南岸外太平洋底发生8.1级强震，震波约2分钟到达墨西哥城。地震发生90秒钟的时间毁掉市中心30%的建筑物。该次地震为墨西哥历史上震级最强、损失最为严重的地震。1985年9月19日晨发生8.1级地震之后，第二天又发生6.5级地震，之后又出现5.5~3.8级余震38次。在这场大地震中，受灾面积32平方公里，8000幢建筑物受到不同程度的破坏，7000多人死亡，1.1万人受伤，30多万人无家可归，经济损失达11亿美元。9月19日被称之为'墨西哥城最悲惨的一天'。",
| "tm":"2017-09-20 17:20:46",
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| "location":"墨西哥",
| "type":"2",
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| "lttd":15.548848379492568,
| "creator":"henry",
| "id":"36c573d8b72045e58e862e242808dc7d",
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| "name":"1985.9.18墨西哥大地震",
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| "nt":"中国地震台网正式测定：2017年09月20日02时14分在墨西哥（北纬18.58度，西经98.47度）发生7.1级地震，震源深度50千米。当地民众自动自发参与救援行动，挖掘碎石瓦砾抢救生还者，也跟其他灾民相互打气、彼此安慰。墨西哥国家救援队负责人普恩特发布消息称，墨西哥首都至少有117人死亡，墨西哥城周边的墨西哥州有12人死亡，莫雷洛斯州有72人死亡，普埃布拉州有43人死亡，格雷罗州有3人死亡，瓦哈卡有一人死亡。",
| "tm":"2017-09-20 17:12:29",
| "lineid":null,
| "geo_yanxing":null,
| "location":"墨西哥",
| "type":"2",
| "is_use":1,
| "lttd":18.58,
| "creator":"henry",
| "id":"193ec273a989449c896c8445db4668bd",
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| "name":"2017墨西哥7.1级地震",
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| "nt":"清康熙七年六月十七日 (1668年7月25日，山东郯城、临沭、临沂交界发生了一个旷古历今的大地震。这次地震是中国历史上地震中最大的地震，震级估计为8.5级，震源深度约36公里，震中烈度12度，死亡人口约5万。据史书记载，以莒县 、临沂县和郯城县的地震灾最重，历史上称为“郯城大地震”，“郯城-临沂大地震”或“郯城-莒县大地震”。莒县的灾情是“官民房屋、寺庙、牌坊、城垣俱倒，周围百余里无一存屋”。郯城的灾情是“城楼垛口、官舍、民房并村落寺观一时俱倒塌如平地”。临沂的灾情是“城郭宫室庙宇公廨一时尽毁，人无完宇”。此震是典型的板块内部大地震 ，其重复期很长。从地质构造上看，有一条深大断裂带自南向北从鲁南地区通过，名为郯城、庐江大断裂。最后一张图片为郯城大地震形成的位于枣庄的熊耳山大裂谷，也是目前我国发现最早的有史料佐证的特大地震山体崩裂遗迹",
| "tm":"2017-09-12 16:22:08",
| "lineid":null,
| "geo_yanxing":null,
| "location":"山东-郯城",
| "type":"2",
| "is_use":1,
| "lttd":35.3,
| "creator":"henry",
| "id":"92483171f4f943b3878e11edf7f1715f",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"1668年8.5级郯城大地震",
| "disaster_geo_yanxing":"1",
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| "nt":"1920年（民国九年）12月16日 ，中国宁夏南部海原县和固原县（当时属甘肃省管辖）一带发生里氏8.5级特大地震，震中位于海原县县城以西哨马营和大沟门之间，地震共造成28.82万人死亡，约30万人受伤。[1] 是中国有地震记载中最高烈度地震，亦是人类有史以来最高烈度地震。全球96个地震监察局录得此次地震，余震维持三年时间。据1949年以后调查，地表断裂带从固原硝河至海原县李俊堡开始向西北发展，经肖家湾、西安州和干盐池至景泰，全长220千米。此震为典型的板块内部大地震，重复期长。",
| "tm":"2017-09-12 10:45:17",
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| "location":"宁夏-海原县",
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| "name":"1920年海原8.5级地震",
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| "nt":"1976年7月28日3时42分53.8秒，中国河北省唐山丰南一带发生了强度里氏7.8级（矩震级7.5级）地震，震中烈度11度，震源深度12千米，地震持续约23秒。地震造成242769人死亡，16.4万人重伤，位列20世纪世界地震史死亡人数第二，仅次于海原地震。",
| "tm":"2017-09-12 10:40:51",
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| "location":"河北-唐山",
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| "nt":"青海省玉树藏族自治州称多县扎朵镇直美村牧场，发生流动形滑坡。",
| "tm":"2017-09-12 10:31:43",
| "lineid":null,
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| "location":"青海省-玉树",
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| "nt":"2017年09月10日22时41分在山东济宁市兖州市发生3.6级地震，震源深度18千米。",
| "tm":"2017-09-10 23:16:28",
| "lineid":null,
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| "location":"山东-兖州",
| "type":"2",
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| "creator":"henry",
| "id":"4adf1b668dc149b68840003e2709104b",
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| "name":"2017年兖州地震",
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| "nt":"黄土坡古滑坡位于巴东县新城区,由变电站滑坡、园艺场滑坡、临江I号崩滑堆积体、II号崩滑堆积体组成。总面积1.35平方公里，体积6934万立方米，是三峡库区最大的易滑坡体。1995年在黄土坡区发生了两次滑坡，危及周边2万多民众生命财产安全，2017年滑坡体上居民全部搬迁。 黄土坡主体为松散的块石土所覆盖,据已有的勘探资料和地质情况推断,基岩地层为中三叠统巴东组第二段(T2b2)和第三段(T2b3).第二段为紫红色钙质泥岩与泥质粉砂岩构成的不等厚互层,分布在斜坡的上部;第三段以青灰色、风化面呈土黄色的泥质灰岩为主,偶夹有薄层的灰绿色钙质泥岩分布，均含碳酸盐矿物5%~10%, 第三段平均含泥质25%~35%。",
| "tm":"2017-08-27 16:56:51",
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| "location":"湖北-巴东",
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| "creator":"henry",
| "id":"3912a5050d2442ffb53855917e5cf713",
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| "name":"黄土坡滑坡",
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| "nt":"中国地质大学（武汉）巴东野外综合试验场。试验场区岩性主要为三叠系巴东组泥质灰岩、泥灰岩及粉砂质泥岩、粉砂岩，是三峡地区典型的易滑地层。受地形地貌、地层岩性、地质构造及水文地质条件控制，本区成为三峡库区滑坡最为发育的典型地段，集中了如黄土坡滑坡、赵树岭滑坡和红石包滑坡等37个大小滑坡。",
| "tm":"2017-08-27 15:21:22",
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| "location":"湖北-巴东",
| "type":"2",
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| "creator":"henry",
| "id":"fd4d4e0b0a25441e86bd3189d735e064",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"巴东野外综合试验场",
| "disaster_geo_yanxing":"1",
| "engineering_type":null,
| "openid":"",
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| "disaster_type":"1",
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| "lgtd":110.3818,
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| "nt":"土石混合体滑坡。基岩为巴东组二段泥灰岩。表层为20m左右的土石混合体层。前缘采用抗滑桩（2m×3m）加固，最大桩长30m；后来由于前缘发生深部滑动，抗滑桩被整体平移8余米。照片中显示的为被移动的抗滑桩。",
| "tm":"2017-08-26 16:20:14",
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| "location":"湖北-巴东",
| "type":"2",
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| "creator":"henry",
| "id":"42991b47f9b44124a2c5ab35933a86d9",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"史家坡滑坡",
| "disaster_geo_yanxing":"2",
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| "openid":"",
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| "disaster_type":"1",
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| "lgtd":110.3278,
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| {
| "nt":"三峡地质灾害。三叠系中统巴东组地层，紫红色泥质岩，官渡口向斜，两岸顺向坡。对面为巴东县城。",
| "tm":"2017-08-26 15:11:55",
| "lineid":null,
| "geo_yanxing":null,
| "location":"湖北-巴东",
| "type":"2",
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| "lttd":31.05713,
| "creator":"henry",
| "id":"5210b7d9251c493d902966ddd034293f",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"巴东华润物流码头",
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| "lgtd":110.3396,
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| "images":"GeologicalDisaster/8a90e53d9285426f8d6e6b9086603481.jpg,GeologicalDisaster/c35a3d2e9670485c9e366fc1d63522f9.jpg,GeologicalDisaster/8014d06dc4a9453c8322efdcfff81147.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"美国-科罗拉多州walden 湿地自然保护区，河流拐歪处有明显的塌岸，但没发现截弯取直的现象。",
| "tm":"2017-08-14 17:52:38",
| "lineid":null,
| "geo_yanxing":null,
| "location":"美国-科罗拉多州walden 自然保护区",
| "type":"2",
| "is_use":1,
| "lttd":39.60317,
| "creator":"wxl15",
| "id":"c56ff31ef8904fd9bf224b8baa098e6d",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"河流塌岸",
| "disaster_geo_yanxing":"2",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"5",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":-106.0778,
| "archaeology_type":null,
| "images":"GeologicalDisaster/f461185c7f2742e1b294e39328e99c2e.jpg,GeologicalDisaster/a422824f239f41b592d8edcc6f02f193.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"2010年4月14日，青海省玉树藏族自治州玉树县发生6次地震最高震级7.1级，发生在7点49分，地震震中位于县城附近。截至2010年5月30日18时，经青海省民政厅、公安厅和玉树州政府按相关程序规定核准，玉树地震已造成2698人遇难，其中已确认身份2687人，无名尸体11具，失踪270人。已确认身份的遇难人员：男性1290人，女性1397人；青海玉树籍2537人，省内非玉树籍54人，外省籍96人（含香港籍贯1人）；遇难学生199人。",
| "tm":"2017-08-13 19:20:26",
| "lineid":null,
| "geo_yanxing":null,
| "location":"青海-玉树藏族自治州",
| "type":"2",
| "is_use":1,
| "lttd":33.1,
| "creator":"henry",
| "id":"58a126e0318a4e269c6cde7cf0fc5d08",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"2014年玉树地震",
| "disaster_geo_yanxing":"1",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"6",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":96.7,
| "archaeology_type":null,
| "images":"GeologicalDisaster/481f4cc0dd334c76adee6cb12b3e3646.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"2017年8月11日13时28分在南海海域附近发生6.5级左右地震，",
| "tm":"2017-08-13 19:16:03",
| "lineid":null,
| "geo_yanxing":null,
| "location":"南海海域",
| "type":"2",
| "is_use":1,
| "lttd":14.38,
| "creator":"henry",
| "id":"769b61962ef445088952088e66539c88",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"2017年南海6.5级地震",
| "disaster_geo_yanxing":"1",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"6",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":120.68,
| "archaeology_type":null,
| "images":"GeologicalDisaster/37cd579bd5e64e42a66405bceced4092.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"2017年8月9日7时27分，在新疆博尔塔拉州精河县发生6.6级地震，震源深度11千米。震中位于精河县托里镇，距精河县城37km，震中区域震感强烈，石河子、昌吉、乌鲁木齐有震感。",
| "tm":"2017-08-13 19:11:45",
| "lineid":null,
| "geo_yanxing":null,
| "location":"新疆-博尔塔拉州",
| "type":"2",
| "is_use":1,
| "lttd":44.27,
| "creator":"henry",
| "id":"125a8c978a9f48738b22ec3104915ad9",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"2017年精河6.6级地震",
| "disaster_geo_yanxing":"1",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"6",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":82.89,
| "archaeology_type":null,
| "images":"GeologicalDisaster/c0dda11c71f6448b9b99e95f84cf5ae3.jpg,GeologicalDisaster/4ee9a09e01264e24bd079f9f0d02ee8e.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"据中国地震台网测定，北京时间2012-06-30 05:07 在新疆维吾尔自治区伊犁哈萨克自治州新源县、巴音郭楞蒙古自治州和静县交界 发生6.6级地震，震源深度7.0公里。",
| "tm":"2017-08-13 19:06:27",
| "lineid":null,
| "geo_yanxing":null,
| "location":"新疆-伊犁",
| "type":"2",
| "is_use":1,
| "lttd":43.4,
| "creator":"henry",
| "id":"f3c5e990f95747c19d3d43dbc8fdb6d5",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"2012年新源地震",
| "disaster_geo_yanxing":"1",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"6",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":84.8,
| "archaeology_type":null,
| "images":"GeologicalDisaster/6c7216b3130d4a5abf6ec4956b6108cb.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"中国地震台网正式测定2017年8月8日21时19分，四川阿坝藏族羌族自治州九寨沟县（北纬33.20度，东经103.82度）发生7.0级地震，震源深度20公里。第三张图为8月9日拍摄的五花海景点。",
| "tm":"2017-08-13 12:26:37",
| "lineid":null,
| "geo_yanxing":null,
| "location":"四川-阿坝州九寨沟",
| "type":"2",
| "is_use":1,
| "lttd":33.2,
| "creator":"henry",
| "id":"7579c394774c4846b826e9235e8dd1d8",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"2017九寨沟7.0级地震",
| "disaster_geo_yanxing":"1",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"6",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":103.82,
| "archaeology_type":null,
| "images":"GeologicalDisaster/c4ae39da9da24da6a686923d458043d2.jpg,GeologicalDisaster/9858bcaa70ef4e3192210b23779365a5.jpg,GeologicalDisaster/44b4723a56be489d9b98952306465159.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"兴海县位于青海省海南藏族自治州西南部，地处“三江源”国家自然保护核心区，该地区属于高原地区，该地区属于高原性气候，半干旱，导致了主要的植被是草原，而且长期处于过度放牧的状态，生态十分脆弱。近年来，该地区成为世界罕见的泥石流多发区域，几乎每年都会发生泥石流，在该地区随处可见大量明显的泥石流沟，深度达上百米的都有几百条。泥石流扇分布于河谷两旁的坡脚处，掩埋了大量的土地和植物。该地区泥石流沟分布广泛，而且每次发生泥石流就会使得泥石流沟不断发展，这样会不断削减生物的活动空间，给环境造成压力。",
| "tm":"2017-08-13 11:34:46",
| "lineid":null,
| "geo_yanxing":null,
| "location":"青海-兴海县同德盆地",
| "type":"2",
| "is_use":1,
| "lttd":35.53399675695728,
| "creator":"2015010312",
| "id":"1f0b2f32149a4926889b63a7db699b01",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"泥石流沟",
| "disaster_geo_yanxing":"2",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"3",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":100.02426004416108,
| "archaeology_type":null,
| "images":"GeologicalDisaster/ce3a05ffe56f4ce6b66b429a9583a7e6.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"同德盆地地区经过很长地质时期的沉积和抬升，有大量的沉积物裸露，而且同德盆地属于黄河的发源地，溯源侵蚀严重，这样就形成了天然的泥石流沟到，沟道两边的堆积物给泥石流提供了丰富的物料。一旦发生强降雨，该地区就会发生泥石流灾害，在该地区形成了大大小小几百个泥石流扇。",
| "tm":"2017-08-12 01:09:07",
| "lineid":null,
| "geo_yanxing":null,
| "location":"青海-兴海县同德盆地",
| "type":"2",
| "is_use":1,
| "lttd":35.512,
| "creator":"2015010312",
| "id":"5e1c41364e744e7fb46cf3bb4d558286",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"泥石流扇",
| "disaster_geo_yanxing":"2",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"3",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":100.143,
| "archaeology_type":null,
| "images":"GeologicalDisaster/182d08488a2642c99f2c06437abd9b22.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"兴海县位于青海省海南藏族自治州西南部，地处“三江源”国家自然保护核心区，该地区属于高原地区，该地区属于高原性气候，半干旱，导致了主要的植被是草原，而且长期处于过度放牧的状态，生态十分脆弱。近年来，该地区成为世界罕见的泥石流多发区域，几乎每年都会发生泥石流，在该地区泥石流堆积物的厚度可以达到十几米，泥石流堆积物大小混杂，分选性差，磨圆度差，成分与发生泥石流的泥石流沟的成分有密切的关系。",
| "tm":"2017-08-12 00:58:48",
| "lineid":null,
| "geo_yanxing":null,
| "location":"青海-兴海县唐乃亥水电站",
| "type":"2",
| "is_use":1,
| "lttd":35.509,
| "creator":"2015010312",
| "id":"ef857a8bdba44537b1198f640184e736",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"泥石流堆积物",
| "disaster_geo_yanxing":"2",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"3",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":100.142,
| "archaeology_type":null,
| "images":"GeologicalDisaster/8de8e1a28c1e4c8e90b652b8afe97cbd.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"由于基坑边坡为土质，且当地遇水较多，有边坡发生滑坡的安全隐患，加上混凝土养护的条件太差，因此工地发生了滑坡，混凝土开裂，需要重新浇混凝土，",
| "tm":"2017-08-11 22:02:20",
| "lineid":null,
| "geo_yanxing":null,
| "location":"广西-容县开发区",
| "type":"2",
| "is_use":1,
| "lttd":22.855,
| "creator":"2015010312",
| "id":"fb3d9eb22a484ca09addd3d6e42cf20e",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"基坑边坡滑坡",
| "disaster_geo_yanxing":"2",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"1",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":110.58,
| "archaeology_type":null,
| "images":"GeologicalDisaster/49e5d3fc43bd4f7c9d36d2d7d45d39bf.jpg,GeologicalDisaster/7bfe5b9390f04878b97ecd7a63b6e37d.jpg,GeologicalDisaster/062deb5bb2134974aad8f6b67a486dbc.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"青海省兴海县境内莫多水电站下游约200m处。莫多水电站位于兴海县城东南方50公里的曲什安镇莫多村峡谷，在莫多水电站下游约200米处，观察到一处规模较大的泥石流沟。沟道两侧山体破碎、滑坡和崩塌作用频繁、水土流失和坡面侵蚀作用强烈，沟道内固体物质积存量大，沟谷上游三面环山、山坡陡峻，沟谷中游山谷狭窄，沟道纵坡降较大，束流特征明显；下游沟口地势开阔，有利于固体物质停积。另外，还观察到扇状堆积体，初步判断为泥石流扇。堆积物以卵石居多，磨圆度较好。",
| "tm":"2017-07-29 23:01:03",
| "lineid":null,
| "geo_yanxing":null,
| "location":"青海省-兴海县莫多水电站",
| "type":"2",
| "is_use":1,
| "lttd":35.51403015706694,
| "creator":"hu-xy15",
| "id":"a44f674f64ac495681deade3956d87a2",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"泥石流沟、泥石流扇",
| "disaster_geo_yanxing":"2",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"3",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":100.01506102753537,
| "archaeology_type":null,
| "images":"GeologicalDisaster/80efe869fd5a4a24805daec454556e54.jpg,GeologicalDisaster/e7d3ca5ce74f4579967262e815eca954.jpg,GeologicalDisaster/5f74d72f0c2742a39e616e7365112257.jpg,GeologicalDisaster/dc7fa1cdb63d4fd88abf5e4b773c4690.jpg,GeologicalDisaster/0a8f2876e0f14969999f1222d4504f5f.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"此处位于慈利县五雷山下一个沿山公路急弯处，从卫星图可清晰看到地质灾害发生地处于两山之间的山谷处。此图为因湖南地区连日暴雨发生泥石流灾害后不久所摄，可以看到大量山石碎屑冲下，沿线房屋的墙壁被泥石流冲毁，一楼已经被淹没，二楼岌岌可危。",
| "tm":"2017-07-19 20:31:29",
| "lineid":null,
| "geo_yanxing":null,
| "location":"湖南-张家界-慈利县黄莲村",
| "type":"2",
| "is_use":1,
| "lttd":29.407631612522657,
| "creator":"henry",
| "id":"b00b6526eafb4e43817753e3816b4a85",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"黄莲村泥石流",
| "disaster_geo_yanxing":"2",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"3",
| "videos":"",
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":111.22076535805266,
| "archaeology_type":null,
| "images":"GeologicalDisaster/03b48edcfaf244b2b835912549b1bdbe.jpg,GeologicalDisaster/2ed89c2b819249b9b67d486e3d25c965.jpg,GeologicalDisaster/7320c0ff1a69413685d46ff89b9a0570.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"泥石流形成区位于高台平原前缘，地层岩性主要为下更新统至全新统冲洪积及 80湖积砂砾卵石和粉土，结构松散，主要由20cm以下大小的卵石和细沙。环境相当恶劣，极容易发生泥石流，基本上每个山沟都是泥石流沟。泥石流痕迹，明显看见树木被掩埋。",
| "tm":"2017-05-05 22:37:10",
| "lineid":null,
| "geo_yanxing":null,
| "location":"青海-兴海县大河坝河",
| "type":"2",
| "is_use":1,
| "lttd":35.514176679695524,
| "creator":"henry",
| "id":"a364942a271741f6a61fbab74f2c1c9f",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"泥石流",
| "disaster_geo_yanxing":"2",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"3",
| "videos":null,
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":100.01525807903711,
| "archaeology_type":null,
| "images":"GeologicalDisaster/a46f5290f32540d7a4c1a318cb174f90.jpg,GeologicalDisaster/40b1db54378b4039b6b265639c2237b3.jpg",
| "adcd":null,
| "decider":"henry",
| "architectural_type":null
| },
| {
| "nt":"唐家山堰塞湖：汶川大地震（2008.5.12）诱发的唐家山滑坡堵塞通口河(湔江)而形成的。堰塞体长803米，宽611米，高82.65至124.4米，方量约2037万立方米，上下游水位差约60米。6月6日，唐家山堰塞湖储水量达超过2.2亿立方米，6月10日1时30分达到最高水位743.1米，最大库容3.2亿立方米，极可能发生溃坝引发下游洪灾，为汶川大地震形成的34处堰塞湖中最危险的一座。于2008年5月23日，人工开挖泄洪槽实现成功泄洪，最大洪峰6800方/s。唐家山滑坡为顺层岩质滑坡，基岩为寒武系下统清平组上部灰黑色薄-中厚层状长石云母粉砂岩、硅质岩、泥灰岩、泥岩互层构成。滑坡山顶高程1580m，坡高900m。",
| "tm":"2017-02-22 08:24:32",
| "lineid":null,
| "geo_yanxing":null,
| "location":"四川省-北川县-通口河",
| "type":"2",
| "is_use":1,
| "lttd":31.84485343339447,
| "creator":"henry",
| "id":"1b52a66811e6493cb8495748c29598b8",
| "geo_gouzao":null,
| "geo_type":null,
| "name":"唐家山堰塞湖",
| "disaster_geo_yanxing":"1",
| "engineering_type":null,
| "openid":"",
| "is_teach":null,
| "disaster_type":"1",
| "videos":null,
| "academyid":null,
| "is_tour":0,
| "country":null,
| "lgtd":104.42901508106476,
| "archaeology_type":null,
| "images":"GeologicalDisaster/cfa674ead76747538fe02e4585b1f35e.jpg,GeologicalDisaster/2a57d726c16e4edd89be5a71d47f03ac.jpg,GeologicalDisaster/cf046791108a4c80b2814786547a0d62.jpg,GeologicalDisaster/a974f42de78e460eacf8af693b6c05b1.jpg,GeologicalDisaster/8737df90fa1640b7b7c488abee0ba87c.jpg",
| "adcd":null,
| "decider":null,
| "architectural_type":null
| }
| ],
| "success":true,
| "stackTrace":null
| }
|
|
