[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"session-user":3,"news-1000000000000000930":4,"\u002Fapi\u002Fnews\u002Flist?categoryId=1000000000000000032&orderByColumn=publishTime&isAsc=desc&pageSize=5":16},null,{"id":5,"articleNo":6,"categoryId":7,"categoryName":8,"title":9,"content":10,"publishTime":11,"isTop":12,"isHot":12,"isRecommend":12,"viewCount":13,"collectCount":14,"updateTime":11,"contentHtml":15},"1000000000000000930","73961","1000000000000000032","水文地质","喀斯特地貌、风成地貌、冰川地貌和海底地貌，一次搞懂！","**喀斯特地貌**\n\n是地下水与地表水对可溶性岩石溶蚀与沉淀，侵蚀与沉积，以及重力崩塌、坍塌、堆积等作用形成的地貌，为中国五大造型地貌之一。\n\n喀斯特地貌分地表和地下两大类，地表有石芽与溶沟，喀斯特漏斗，落水洞，溶蚀洼地，喀斯特盆地与喀斯特平原，峰丛、峰林与孤峰；地下有溶洞与地下河，暗湖。\n\n喀斯特地貌在中国分布最广，其集中分布于桂、黔、滇等省区，川、渝、湘、晋、甘、藏等省区部分地区亦有分布。\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F9cbf44fc62b707ab46fca2ac513d6865.png)![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002Fbc5940a1b63e7b026114de02ee8bd18b.jpg)![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F24dacd98b8bd04a90f6a1dca4485d4b7.jpg)![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F1ecb640c26568beef25d4e72018afc25.jpg)![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002Fa985d5597754f2bd0b12c2756969a829.jpg)![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F8b7db1cb4226a9d8e1f2ffd3b16caf36.jpg)\n\n**风成地貌**\n\n在风对地面物质进行吹蚀、搬运和堆积作用的过程中所形成的各种风蚀地貌和风积地貌，统称为风成地貌。世界上的风成地貌主要分布在干旱和半干旱气候区。我国西北地区也有较大面积的风成地貌分布。\n\n**冰川地貌**\n\n由冰川作用塑造的地貌。属于气候地貌范畴。地球陆地表面有11%的面积为现代冰川覆盖，主要分布在极地、中低纬的高山和高原地区。第四纪冰期，欧、亚、北美的大陆冰盖连绵分布，曾波及比今日更为宽广的地域，给地表留下了大量冰川遗迹。\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F4d1acbaa35bf52e710a1d33276f3ee14.jpg)\n\n如果冰川\n\n消融的速度低于积累的速度那么冰川将会向前扩展冰川逐渐加厚\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F26b483e87a0ebe8d169dbca584d972a7.gif)\n\n如果冰川消融的速度超过了积累的速度那么冰川将会向起点后退冰川逐渐变薄\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F61163b6625cb7f348d31dc6dd40421ac.gif)\n如果冰川消融的速度与积累的速度大致相同那么冰川尖端位置不变将会不断产生冰碛物沉积\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F894c300ddf9ff01491984b35742844bb.gif)\n\n**冰川侵蚀地貌示意图**\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F377d9759df2d1e5a19c018930af5b8c7.jpg)\n\n冰川侵蚀原理\n\n**\n\n▼\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F3fa1336fb5a0a7ca6ef973980075a9b8.gif)\n\nU型谷的形成\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F308454a9e52f6e546b552eb183eb8b7a.gif)\n\n冰川侵蚀地貌成因整体示意图\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002Fb6e8b05d16d04c93eeb174a7e215a4e4.jpg)\n\n 冰川侵蚀地貌成因整体示意图\n\n▼\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F6be6b278960dd2eafcc54fdb5f63d150.jpg)\n\n角峰形成示意图\n\n▼\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002Fa98f1335d571f84a3baedfb22dc8037d.jpg)\n\n塔状尖峰示意图\n\n▼\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F9cf2bf5b38ae8550fe77441076b2b541.jpg)\n\n峡湾的形成示意图，来源不明\n\n▼\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F898dc33dd6555034d4bdcc21f7f3f24a.jpg)\n\n羊背石形成原理示意图\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002Fea97bb5a8e7b72936d8c4b8bb4047aeb.jpg)\n\n**冰川堆积地貌示意图**\n\n冰川沉积原理示意图\n\n▼\n\n![](https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F33a36a828d09382e59754707f47a5235.gif)\n\n**海底地貌**\n\n海水覆盖下的固体地球表面形态的总称。海底有高耸的海山，起伏的海丘，绵延的海岭，深邃的海沟，也有坦荡的深海平原。纵贯大洋中部的大洋中脊，绵延 8 万千米，宽数百至数千千米，总面积堪与全球陆地相比。大洋最深点11034 米，位于太平洋马里亚纳海沟，超过了陆上最高峰珠穆朗玛峰的海拔高度（ 8846.27米 ）。深海平原坡度小于千分之一，其平坦程度超过大陆平原。整个海底可分为大陆边缘、大洋盆地和大洋中脊三大基本地貌单元，及若干次一级的海底地貌单元。①大陆边缘 ②大洋盆地 ③大洋中脊。\n\n**","2022-11-20T19:05:48+08:00","N",4448,0,"\u003Cp>\u003Cstrong>喀斯特地貌\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>是地下水与地表水对可溶性岩石溶蚀与沉淀，侵蚀与沉积，以及重力崩塌、坍塌、堆积等作用形成的地貌，为中国五大造型地貌之一。\u003C\u002Fp>\n\u003Cp>喀斯特地貌分地表和地下两大类，地表有石芽与溶沟，喀斯特漏斗，落水洞，溶蚀洼地，喀斯特盆地与喀斯特平原，峰丛、峰林与孤峰；地下有溶洞与地下河，暗湖。\u003C\u002Fp>\n\u003Cp>喀斯特地貌在中国分布最广，其集中分布于桂、黔、滇等省区，川、渝、湘、晋、甘、藏等省区部分地区亦有分布。\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F9cbf44fc62b707ab46fca2ac513d6865.png\" alt=\"\">\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002Fbc5940a1b63e7b026114de02ee8bd18b.jpg\" alt=\"\">\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F24dacd98b8bd04a90f6a1dca4485d4b7.jpg\" alt=\"\">\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F1ecb640c26568beef25d4e72018afc25.jpg\" alt=\"\">\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002Fa985d5597754f2bd0b12c2756969a829.jpg\" alt=\"\">\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F8b7db1cb4226a9d8e1f2ffd3b16caf36.jpg\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cstrong>风成地貌\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>在风对地面物质进行吹蚀、搬运和堆积作用的过程中所形成的各种风蚀地貌和风积地貌，统称为风成地貌。世界上的风成地貌主要分布在干旱和半干旱气候区。我国西北地区也有较大面积的风成地貌分布。\u003C\u002Fp>\n\u003Cp>\u003Cstrong>冰川地貌\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>由冰川作用塑造的地貌。属于气候地貌范畴。地球陆地表面有11%的面积为现代冰川覆盖，主要分布在极地、中低纬的高山和高原地区。第四纪冰期，欧、亚、北美的大陆冰盖连绵分布，曾波及比今日更为宽广的地域，给地表留下了大量冰川遗迹。\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F4d1acbaa35bf52e710a1d33276f3ee14.jpg\" alt=\"\">\u003C\u002Fp>\n\u003Cp>如果冰川\u003C\u002Fp>\n\u003Cp>消融的速度低于积累的速度那么冰川将会向前扩展冰川逐渐加厚\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F26b483e87a0ebe8d169dbca584d972a7.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>如果冰川消融的速度超过了积累的速度那么冰川将会向起点后退冰川逐渐变薄\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F61163b6625cb7f348d31dc6dd40421ac.gif\" alt=\"\">\n如果冰川消融的速度与积累的速度大致相同那么冰川尖端位置不变将会不断产生冰碛物沉积\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F894c300ddf9ff01491984b35742844bb.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cstrong>冰川侵蚀地貌示意图\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F377d9759df2d1e5a19c018930af5b8c7.jpg\" alt=\"\">\u003C\u002Fp>\n\u003Cp>冰川侵蚀原理\u003C\u002Fp>\n\u003Cp>**\u003C\u002Fp>\n\u003Cp>▼\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F3fa1336fb5a0a7ca6ef973980075a9b8.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>U型谷的形成\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F308454a9e52f6e546b552eb183eb8b7a.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>冰川侵蚀地貌成因整体示意图\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002Fb6e8b05d16d04c93eeb174a7e215a4e4.jpg\" alt=\"\">\u003C\u002Fp>\n\u003Cp>冰川侵蚀地貌成因整体示意图\u003C\u002Fp>\n\u003Cp>▼\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F6be6b278960dd2eafcc54fdb5f63d150.jpg\" alt=\"\">\u003C\u002Fp>\n\u003Cp>角峰形成示意图\u003C\u002Fp>\n\u003Cp>▼\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002Fa98f1335d571f84a3baedfb22dc8037d.jpg\" alt=\"\">\u003C\u002Fp>\n\u003Cp>塔状尖峰示意图\u003C\u002Fp>\n\u003Cp>▼\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F9cf2bf5b38ae8550fe77441076b2b541.jpg\" alt=\"\">\u003C\u002Fp>\n\u003Cp>峡湾的形成示意图，来源不明\u003C\u002Fp>\n\u003Cp>▼\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F898dc33dd6555034d4bdcc21f7f3f24a.jpg\" alt=\"\">\u003C\u002Fp>\n\u003Cp>羊背石形成原理示意图\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002Fea97bb5a8e7b72936d8c4b8bb4047aeb.jpg\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cstrong>冰川堆积地貌示意图\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>冰川沉积原理示意图\u003C\u002Fp>\n\u003Cp>▼\u003C\u002Fp>\n\u003Cp>\u003Cimg src=\"https:\u002F\u002Ffile.sinosite.com.cn\u002Fsinosite-file\u002Fnews\u002Fold\u002F20221120\u002F33a36a828d09382e59754707f47a5235.gif\" alt=\"\">\u003C\u002Fp>\n\u003Cp>\u003Cstrong>海底地貌\u003C\u002Fstrong>\u003C\u002Fp>\n\u003Cp>海水覆盖下的固体地球表面形态的总称。海底有高耸的海山，起伏的海丘，绵延的海岭，深邃的海沟，也有坦荡的深海平原。纵贯大洋中部的大洋中脊，绵延 8 万千米，宽数百至数千千米，总面积堪与全球陆地相比。大洋最深点11034 米，位于太平洋马里亚纳海沟，超过了陆上最高峰珠穆朗玛峰的海拔高度（ 8846.27米 ）。深海平原坡度小于千分之一，其平坦程度超过大陆平原。整个海底可分为大陆边缘、大洋盆地和大洋中脊三大基本地貌单元，及若干次一级的海底地貌单元。①大陆边缘 ②大洋盆地 ③大洋中脊。\u003C\u002Fp>\n\u003Cp>**\u003C\u002Fp>\n",{"items":17,"total":38,"pageNum":54,"pageSize":55},[18,25,32,39,47],{"id":19,"articleNo":20,"categoryId":7,"categoryName":8,"title":21,"summary":22,"publishTime":23,"isTop":12,"isHot":12,"isRecommend":12,"viewCount":24,"collectCount":14,"updateTime":23},"1000000000000001244","74488","涨知识：看不见的地下水","水，是生命之源，在人类的生存与发展进程中占据着无可替代的关键地位。而地下水，作为地球上水资源储存库之一，对于全球水资源的稳定供应和生态平衡的维系，有着深远影响。","2026-04-27T10:57:00+08:00",124,{"id":26,"articleNo":27,"categoryId":7,"categoryName":8,"title":28,"summary":29,"publishTime":30,"isTop":12,"isHot":12,"isRecommend":12,"viewCount":31,"collectCount":14,"updateTime":30},"1000000000000001243","74487","土壤“八大问题”，你知道几个！","土壤“八大问题”-板、馋、贫、浅、酸、咸、脏、杂。","2026-04-27T09:07:43+08:00",104,{"id":33,"articleNo":34,"categoryId":7,"categoryName":8,"title":35,"summary":36,"publishTime":37,"isTop":12,"isHot":12,"isRecommend":12,"viewCount":38,"collectCount":14,"updateTime":37},"1000000000000001242","74486","5分钟学会判断土壤健康，如果您家的土壤有盐碱、酸化、板结等问题，请速看！","5 分钟学会判断土壤健康，如果您家的土壤有盐碱、酸化、板结等问题，请速看！！","2026-04-27T08:51:59+08:00",116,{"id":40,"articleNo":41,"categoryId":7,"categoryName":8,"title":42,"summary":43,"publishTime":44,"isTop":12,"isHot":12,"isRecommend":12,"viewCount":45,"collectCount":14,"updateTime":46},"1000000000000001240","74484","《生态环境法典》“固体废物污染防治”分编与《固废法》对比","《生态环境法典》第二编第六分编“固体废物污染防治”与《固体废物污染环境防治法》进行对比","2026-03-31T09:12:16+08:00",2,"2026-03-31T09:13:25+08:00",{"id":48,"articleNo":49,"categoryId":7,"categoryName":8,"title":50,"summary":51,"publishTime":52,"isTop":12,"isHot":12,"isRecommend":12,"viewCount":53,"collectCount":14,"updateTime":52},"1000000000000001239","74483","《生态环境法典》“水污染防治”分编与《水污染防治法》对比","本次推文将《生态环境法典》第二编第三分编“水污染防治”与《水污染防治法》进行对比。","2026-03-30T10:44:27+08:00",204,1,5]