The torrential rain may flood the low-lying land out.

这场骤雨有可能把低洼地淹没。

The cottage is in that hollow.

村舍在那片洼地。

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

表层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势相对较低洼风化壳表面，形成一些沟、洞、缝、蚀洼地、蚀漏斗及落水洞等，其充填物主要为地表残积物和洞壁塌积物。

The karst depression belongs to the accumulative area of surface water and subdrainage area of subsurface water, the karstification is relatively week, and reservoirs are undeveloped.

斜坡和洼地为地表水汇集区及地下水排泄区，用相对较弱，储层不发育。

The torrential rain may flood the low-lying land out.

这场骤雨有可能把低洼地淹没。

The cottage is in that hollow.

村舍在那片洼地。

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势相对较低洼风化壳表面，形成一些溶沟、溶洞、溶缝、溶蚀洼地、溶蚀漏斗及落洞等，其充填物主要为地表残积物和洞壁塌积物。

The karst depression belongs to the accumulative area of surface water and subdrainage area of subsurface water, the karstification is relatively week, and reservoirs are undeveloped.

岩溶斜坡和岩溶洼地为地表汇集区及地泄区，岩溶作用相对较弱，储层不发育。

The torrential rain may flood the low-lying land out.

这场骤雨有可能把低洼淹没。

The cottage is in that hollow.

村舍在那片洼。

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，风化淋滤及表径流改造而破碎，短距离搬运堆积于对较低洼风化壳表，一些溶沟、溶洞、溶缝、溶蚀洼、溶蚀漏斗及落水洞等，其充填物主要为表残积物和洞壁塌积物。

The karst depression belongs to the accumulative area of surface water and subdrainage area of subsurface water, the karstification is relatively week, and reservoirs are undeveloped.

岩溶斜坡和岩溶洼为表水汇集区及下水排泄区，岩溶作用对较弱，储层不发育。

The torrential rain may flood the low-lying land out.

这场骤雨有可能淹没。

The cottage is in that hollow.

村舍在那片。

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，风化淋滤及表径流改造而破碎，短距离搬运堆积于势相对较风化壳表面，形成一些溶沟、溶洞、溶缝、溶蚀、溶蚀漏斗及落水洞等，其充填物主要表残积物和洞壁塌积物。

The karst depression belongs to the accumulative area of surface water and subdrainage area of subsurface water, the karstification is relatively week, and reservoirs are undeveloped.

岩溶斜坡和岩溶表水汇集区及下水排泄区，岩溶作用相对较弱，储层不发育。

The torrential rain may flood the low-lying land out.

这场骤雨有可能把低洼地淹没。

The cottage is in that hollow.

村舍在那片洼地。

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

表层岩溶带位于化壳表层，化淋滤及地表径流改造而破碎，短距离搬运堆积于地势相对较低洼化壳表面，形成一些溶沟、溶洞、溶缝、溶蚀洼地、溶蚀漏斗及落水洞等，物主要为地表残积物和洞壁塌积物。

The karst depression belongs to the accumulative area of surface water and subdrainage area of subsurface water, the karstification is relatively week, and reservoirs are undeveloped.

岩溶斜坡和岩溶洼地为地表水汇集区及地下水排泄区，岩溶作用相对较弱，储层不发育。

The torrential rain may flood the low-lying land out.

这场骤雨有可能把低洼淹没。

The cottage is in that hollow.

村舍在那片洼。

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

表层岩溶带位风化壳表层上部，风化淋滤及表径流改造而破碎，短距离搬运堆积相对较低洼风化壳表面，些溶沟、溶洞、溶缝、溶蚀洼、溶蚀漏斗及落水洞等，其充填物主要为表残积物和洞壁塌积物。

The karst depression belongs to the accumulative area of surface water and subdrainage area of subsurface water, the karstification is relatively week, and reservoirs are undeveloped.

岩溶斜坡和岩溶洼为表水汇集区及下水排泄区，岩溶作用相对较弱，储层不发育。

The torrential rain may flood the low-lying land out.

这场骤雨有可能把低洼地淹没。

The cottage is in that hollow.

村舍在那片洼地。

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

表层岩带位于风化壳表层上部，风化淋滤及地表径流改造而破碎，短运堆积于地势相对较低洼风化壳表面，形成一些沟、、缝、蚀洼地、蚀漏斗及落水等，其充填物主要为地表残积物和壁塌积物。

The karst depression belongs to the accumulative area of surface water and subdrainage area of subsurface water, the karstification is relatively week, and reservoirs are undeveloped.

岩斜坡和岩洼地为地表水汇集区及地下水排泄区，岩作用相对较弱，储层不发育。

The torrential rain may flood the low-lying land out.

这场骤雨有可能把低洼淹没。

The cottage is in that hollow.

村舍在那片洼。

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，风化淋滤及表径流改造而破碎，短距离搬运堆积于对较低洼风化壳表，一些溶沟、溶洞、溶缝、溶蚀洼、溶蚀漏斗及落水洞等，其充填物主要为表残积物和洞壁塌积物。

The karst depression belongs to the accumulative area of surface water and subdrainage area of subsurface water, the karstification is relatively week, and reservoirs are undeveloped.

岩溶斜坡和岩溶洼为表水汇集区及下水排泄区，岩溶作用对较弱，储层不发育。

The torrential rain may flood the low-lying land out.

这场骤雨有可能把低洼地淹没。

The cottage is in that hollow.

村舍在那片洼地。

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

表层位于风化壳表层上部，风化淋滤及地表径流改造而破碎，短距离搬运堆于地势相对较低洼风化壳表面，形成一些沟、洞、缝、蚀洼地、蚀漏斗及落水洞等，其充填主要为地表残洞壁塌。

The karst depression belongs to the accumulative area of surface water and subdrainage area of subsurface water, the karstification is relatively week, and reservoirs are undeveloped.

斜坡洼地为地表水汇集区及地下水排泄区，作用相对较弱，储层不发育。