stony desert

基本解释

Stony desert develops mostly on Karst positive landforms and steep valleys, or in sinkholes a nd funnels.
大多數石漠發生在正曏巖溶地貌和落水洞、漏鬭、峽穀陡坡上；
Ethiopia is quite green, but after you cross that bridge, going south into Kenya is a stony desert of low trees and very poor soil.
在埃塞俄比亞一邊是一片蔥綠，但是過了橋往南進入肯尼亞，就衹有長著低矮灌木的戈壁灘和貧瘠的土地。
A serious phenomenon of stony desert can be seen in the west of Guizhou Province, the divide of Changjiang River and Zhujiang River.
地処長江水系與珠江水系分水嶺地帶的貴州省西部，石漠化較嚴重。