巨型的地表钙华坡谷，蜿蜒于天然林和石山冰峰之间，宛若金色“巨龙”腾游天地。
The sloping valley goes along between the forests and ice peaks like a huge dragon flying in the sky.
模拟再现了陕北宅基边坡伤亡性黄土崩塌的形成机制，验证了治理此类崩塌的有效措施—建成的宅基边坡谷缘坡度不得大于天然谷缘坡度。
The mechanism and main prevention-cure measure of cutting the top of loess slope according to its nature gradient for the landfall are quantitatively reformed and simulated.
山越来越高，坡越来越大，谷越来越深。
Mountain rising, increasing slope, valley deeper and deeper.
低水位时期坡折带控制了下切谷-低位三角洲沉积体系的发育。
The depositional slope-break belt controls the development of sediment system of eroded valley-low stand delta.
形成机制是流水溯源侵蚀—岩石块体崩塌—谷坡后退。
The formation mechanism is the flowing water trace to the source erosion-rock collapse-ancient slope withdrawal.
木与林厂址：长沙市河西桐梓坡西路麓谷国际工业园，园区环境优雅，工厂提供24小时服务。
Location: West of Tongzi slopes road, Changsha Lugu high~tech industry garden, elegant surroundings, 24-hour service provided by the factory.
木与林厂址：长沙市河西桐梓坡西路麓谷国际工业园，园区环境优雅，工厂提供24小时服务。
Location: West of Tongzi slopes road, Changsha Lugu high~tech industry garden, elegant surroundings, 24-hour service provided by the factory.
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