The railroad was blocked by a landslide.

塌方把铁路。

The village was destroyed by a landslide.

坡摧毀村庄。

According to material composition, landslides in this area can be divided into two categories: rockslide and sedentary-slope wash landslide.

本文对该地区的坡进行分类。依据该地区坡物质组成特征将坡分为岩质坡和坡—残积物坡两类。

The general formula about the calculation of downslide force and resistance to sliding in the arbitrary unit of landslide is deduced in the digital landform image.

讨论坡动态方向稳定性系数的概念，并在此基础上定义坡的动方向和坡的稳定性系数。

After the Three Gorges Reservoir impounded, due to the rise of ground water, the flabbiness layers in landslides will become soft and collapse when they meet water.

三峡库区蓄水后,由于水位上升坡地区的软弱层遇到水就会变软并引起塌。

The tourist landscape in Xi an Cuihua Mountain, is generated from a large paleo-avalanchine landslide, with the special deposit structures showing indirectly information of high speed block movement.

西安翠华山风景地貌由古崩塌性坡体高速运动堆积而成,堆积体存在一些反映其运动和动力状况的沉积特征。

The railroad was blocked by a landslide.

方把铁路堵塞了。

The village was destroyed by a landslide.

摧毀了村庄。

According to material composition, landslides in this area can be divided into two categories: rockslide and sedentary-slope wash landslide.

本文对该地区的进行了分类。依据该地区物质组成特征将分为岩质和—残积物两类。

The general formula about the calculation of downslide force and resistance to sliding in the arbitrary unit of landslide is deduced in the digital landform image.

讨论了动态方向稳定性系数的概念，并在此定义了的动方向和的稳定性系数。

After the Three Gorges Reservoir impounded, due to the rise of ground water, the flabbiness layers in landslides will become soft and collapse when they meet water.

三峡库区蓄水后,由于水位升地区的软弱层遇到水就会变软并引起。

The tourist landscape in Xi an Cuihua Mountain, is generated from a large paleo-avalanchine landslide, with the special deposit structures showing indirectly information of high speed block movement.

西安翠华山风景地貌由古崩性体高速运动堆积而成,堆积体存在一些反映其运动和动力状况的沉积特征。

The railroad was blocked by a landslide.

塌方把铁路堵塞了。

The village was destroyed by a landslide.

摧毀了村庄。

According to material composition, landslides in this area can be divided into two categories: rockslide and sedentary-slope wash landslide.

本文对该地区进行了分类。依据该地区物质组成特征将分为岩质和—残积物两类。

The general formula about the calculation of downslide force and resistance to sliding in the arbitrary unit of landslide is deduced in the digital landform image.

讨论了动态方向稳定性系数概念，并在此基础上定义了动方向和稳定性系数。

After the Three Gorges Reservoir impounded, due to the rise of ground water, the flabbiness layers in landslides will become soft and collapse when they meet water.

三峡库区蓄水后,由于水位上升地区软弱层遇到水就会变软并引起塌。

The tourist landscape in Xi an Cuihua Mountain, is generated from a large paleo-avalanchine landslide, with the special deposit structures showing indirectly information of high speed block movement.

西安翠华山风景地貌由古崩塌性体高速运动堆积而成,堆积体存在一些反映其运动和动力状况沉积特征。

The railroad was blocked by a landslide.

方把铁路堵塞了。

The village was destroyed by a landslide.

滑摧毀了村庄。

According to material composition, landslides in this area can be divided into two categories: rockslide and sedentary-slope wash landslide.

本文对该地区的滑进行了分类。依据该地区滑物质组成特征将滑分为岩质滑和—残积物滑两类。

The general formula about the calculation of downslide force and resistance to sliding in the arbitrary unit of landslide is deduced in the digital landform image.

讨论了滑动态方向稳定性系数的概念，并在此基础上定义了滑的滑动方向和滑的稳定性系数。

After the Three Gorges Reservoir impounded, due to the rise of ground water, the flabbiness layers in landslides will become soft and collapse when they meet water.

三峡区蓄水后,由于水位上升滑地区的软弱层遇到水就会变软并引起滑。

The tourist landscape in Xi an Cuihua Mountain, is generated from a large paleo-avalanchine landslide, with the special deposit structures showing indirectly information of high speed block movement.

西安翠华山风景地貌由古崩性滑体高速运动堆积而成,堆积体存在一些反映其运动和动力状况的沉积特征。

The railroad was blocked by a landslide.

塌方把铁路堵塞了。

The village was destroyed by a landslide.

坡摧毀了村庄。

According to material composition, landslides in this area can be divided into two categories: rockslide and sedentary-slope wash landslide.

本文对该地区的坡进行了分类。依据该地区坡质组成特征将坡分为岩质坡和坡—残坡两类。

The general formula about the calculation of downslide force and resistance to sliding in the arbitrary unit of landslide is deduced in the digital landform image.

讨论了坡动态方向稳定性系数的概念，并在此基础上定义了坡的动方向和坡的稳定性系数。

After the Three Gorges Reservoir impounded, due to the rise of ground water, the flabbiness layers in landslides will become soft and collapse when they meet water.

三峡库区蓄水后,由于水位上升坡地区的软弱层遇到水就会变软并引起塌。

The tourist landscape in Xi an Cuihua Mountain, is generated from a large paleo-avalanchine landslide, with the special deposit structures showing indirectly information of high speed block movement.

西安翠华山风景地貌由古崩塌性坡体高速运动堆而成,堆体存在一些反映其运动和动力状况的沉特征。

The railroad was blocked by a landslide.

塌方把铁路堵塞。

The village was destroyed by a landslide.

滑坡摧毀村庄。

According to material composition, landslides in this area can be divided into two categories: rockslide and sedentary-slope wash landslide.

本文对该地区的滑坡进类。依据该地区滑坡物质组成特征将滑坡为岩质滑坡和坡—残积物滑坡两类。

The general formula about the calculation of downslide force and resistance to sliding in the arbitrary unit of landslide is deduced in the digital landform image.

讨论滑坡动态方向稳定性系数的概念，并在此基础上定义滑坡的滑动方向和滑坡的稳定性系数。

After the Three Gorges Reservoir impounded, due to the rise of ground water, the flabbiness layers in landslides will become soft and collapse when they meet water.

三峡库区蓄后,由于位上升滑坡地区的软弱层遇到就会变软并引起滑塌。

The tourist landscape in Xi an Cuihua Mountain, is generated from a large paleo-avalanchine landslide, with the special deposit structures showing indirectly information of high speed block movement.

西安翠华山风景地貌由古崩塌性滑坡体高速运动堆积而成,堆积体存在一些反映其运动和动力状况的沉积特征。

The railroad was blocked by a landslide.

塌方把铁路堵塞。

The village was destroyed by a landslide.

滑坡摧毀。

According to material composition, landslides in this area can be divided into two categories: rockslide and sedentary-slope wash landslide.

本文该地区的滑坡进行分类。依据该地区滑坡物质组成特征将滑坡分为岩质滑坡和坡—残积物滑坡两类。

The general formula about the calculation of downslide force and resistance to sliding in the arbitrary unit of landslide is deduced in the digital landform image.

讨论滑坡动态方向稳定性系数的概念，并在此基础上定义滑坡的滑动方向和滑坡的稳定性系数。

After the Three Gorges Reservoir impounded, due to the rise of ground water, the flabbiness layers in landslides will become soft and collapse when they meet water.

三峡库区蓄水后,由于水位上升滑坡地区的软弱层遇到水就会变软并引起滑塌。

The tourist landscape in Xi an Cuihua Mountain, is generated from a large paleo-avalanchine landslide, with the special deposit structures showing indirectly information of high speed block movement.

西安翠华山风景地貌由古崩塌性滑坡体高速运动堆积而成,堆积体存在一些反映其运动和动力状况的沉积特征。

The railroad was blocked by a landslide.

塌方把铁路堵塞了。

The village was destroyed by a landslide.

滑摧毀了村庄。

According to material composition, landslides in this area can be divided into two categories: rockslide and sedentary-slope wash landslide.

本文对该地区滑进行了分类。依据该地区滑物质组成特征将滑分为岩质滑和—残积物滑两类。

The general formula about the calculation of downslide force and resistance to sliding in the arbitrary unit of landslide is deduced in the digital landform image.

讨论了滑动态方向定性系数概念，并在此基础上定义了滑滑动方向和滑定性系数。

After the Three Gorges Reservoir impounded, due to the rise of ground water, the flabbiness layers in landslides will become soft and collapse when they meet water.

三峡库区蓄水后,由于水位上升滑地区软弱层遇到水就会变软并引起滑塌。

The tourist landscape in Xi an Cuihua Mountain, is generated from a large paleo-avalanchine landslide, with the special deposit structures showing indirectly information of high speed block movement.

西安翠华山风景地貌由古崩塌性滑体高速运动堆积而成,堆积体存在一些反映其运动和动力状况沉积特征。

The railroad was blocked by a landslide.

塌把铁路堵塞了。

The village was destroyed by a landslide.

滑坡摧毀了村庄。

According to material composition, landslides in this area can be divided into two categories: rockslide and sedentary-slope wash landslide.

本文对该地区的滑坡进行了分类。依据该地区滑坡物质组成特征将滑坡分为岩质滑坡和坡—残积物滑坡两类。

The general formula about the calculation of downslide force and resistance to sliding in the arbitrary unit of landslide is deduced in the digital landform image.

讨论了滑坡动稳定性系的概念，并在此基础上定义了滑坡的滑动和滑坡的稳定性系。

After the Three Gorges Reservoir impounded, due to the rise of ground water, the flabbiness layers in landslides will become soft and collapse when they meet water.

三峡库区蓄水后,由于水位上升滑坡地区的软弱层遇到水就会变软并引起滑塌。

The tourist landscape in Xi an Cuihua Mountain, is generated from a large paleo-avalanchine landslide, with the special deposit structures showing indirectly information of high speed block movement.

西安翠华山风景地貌由古崩塌性滑坡体高速运动堆积而成,堆积体存在些反映其运动和动力状况的沉积特征。