The ground falls away abruptly to the right.

右边的地陡降。

East of the gorge leveled out.

峡谷东面地变得平坦起来。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩于风化壳表层上部，风化淋滤及地表径流改造而破碎，短距离搬运堆积于地相对较低洼的风化壳表面，形成一些沟、、缝、蚀洼地、蚀漏斗及落，其充填物主要为地表残积物和壁塌积物。

The ground falls away abruptly to the right.

右边的地陡降。

East of the gorge leveled out.

峡谷东面地变得平坦起来。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩溶风化壳表层上部，风化淋滤及地表径流改造而破碎，短距离搬运堆积地相对较低洼的风化壳表面，形成一些溶沟、溶、溶缝、溶蚀洼地、溶蚀漏斗及等，其充填物主要为地表残积物和壁塌积物。

The ground falls away abruptly to the right.

右边的地陡降。

East of the gorge leveled out.

峡谷东面地变得平坦起来。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩带位于壳表层上，淋滤及地表径流改造而破碎，短距离搬运堆积于地相对较低的壳表面，形成一些沟、洞、缝、地、漏斗及落水洞等，其充填物主要为地表残积物和洞壁塌积物。

The ground falls away abruptly to the right.

右边的地陡降。

East of the gorge leveled out.

峡谷东面地变得平坦起来。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩溶带位于风化壳表层上部，风化淋滤及地表径流改造而破碎，短距离搬于地相对的风化壳表面，形成一些溶沟、溶洞、溶缝、溶蚀地、溶蚀漏斗及落水洞等，其充填物主要为地表残物和洞壁塌物。

The ground falls away abruptly to the right.

右边的地陡。

East of the gorge leveled out.

东面地变得平坦起来。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩溶带位于风化壳表层上部，风化淋滤及地表径流改造而破碎，短距离搬运堆积于地相对较低洼的风化壳表面，形成一些溶沟、溶、溶缝、溶蚀洼地、溶蚀漏斗及落水等，其充填物主要为地表残积物和积物。

The ground falls away abruptly to the right.

右边的地陡降。

East of the gorge leveled out.

峡谷东面地变得平坦起。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

岩溶带位于风化壳上部，风化淋滤及地径流改造而破碎，短距离搬运堆积于地相对较低洼的风化壳面，形成一些溶沟、溶洞、溶缝、溶蚀洼地、溶蚀漏斗及落水洞等，其主要为地残积和洞壁塌积。

The ground falls away abruptly to the right.

右边的地陡降。

East of the gorge leveled out.

峡谷东面地变得来。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩溶带位于风化壳表层上部，风化淋滤及地表径流改造而破碎，短距离搬运堆积于地相对较低洼的风化壳表面，形成一些溶沟、溶洞、溶缝、溶蚀洼地、溶蚀漏斗及落水洞等，其充填物地表残积物和洞壁塌积物。

The ground falls away abruptly to the right.

右边的陡降。

East of the gorge leveled out.

峡谷东面坦起来。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

层岩溶带位于风化壳层上部，风化淋滤及径流改造而破碎，短距离搬运堆积于相对较低洼的风化壳面，形成一些溶沟、溶洞、溶缝、溶蚀洼、溶蚀漏斗及落水洞等，其充填物主要残积物和洞壁塌积物。

The ground falls away abruptly to the right.

右边的地陡降。

East of the gorge leveled out.

峡谷东面地变得来。

Hypergenesis palaeokarst usually manifests distinct vertical zoning rule which divides into epikarst zone, vadose zone and phreatic zone.

表层岩溶带位于风化壳表层上部，风化淋滤及地表径流改造而破碎，短距离搬运堆积于地相对较低洼的风化壳表面，形成一些溶沟、溶洞、溶缝、溶蚀洼地、溶蚀漏斗及落水洞等，其充填物地表残积物和洞壁塌积物。