n.喀斯特，喀斯特地貌（石灰岩地区常见的地形）
n.（Karst）（荷）卡斯特（人名）
Karst landscapes differ because of geology and climate.───喀斯特景观会因地质和气候不同而异。
There are karst caves in Guilin.───桂林有溶洞。
The principal karst features are the karst hills, dry valley, the grike and so on.───主要岩溶形态有岩溶丘陵、干谷、岩溶沟等。
Karst said the bookstore, located near the city's new library and concert hall, will be the biggest of its kind in the world.───卡斯特说，中心书城与深圳市新图书馆和音乐厅相邻，是世界上最大的同类书城。
The sea-level fluctuation was an important controlling factor for karst carbonate reservoir development in the Early Paleozoic Tarim Basin.───海平面变化是控制塔里木盆地下古生界岩溶储层发育的一个重要的因素。
As I was sitting on the boat, the Karst mountain scenery came into view.───当我坐在船上时，喀斯特地貌的山峦映入眼帘。
The building ground belings to Karst area with various and a large number of caves, and with developed bedrock fissures.───该工程地处岩溶地区，基岩裂隙极为发育且溶洞表现形式多样，伴随大量土洞出现。
The prediction theory and forecast method of tunnel water gushing in karst areas have long been a difficult hydrogeological problem.───岩溶地区隧道地下水涌水预测方法和理论是长期以来难以突破的水文地质难题。
I cannot find anywhere though: how will the Karst topography along hillsides of the Appalachians behave during the New Madrid release?───虽然我到处都找不到：在新马德里断层带释放压力期间，沿着阿巴拉契亚山区山坡的卡斯特地形会怎么样？
Karst landforms related more specifically to fluvial activity are discussed in Chapter 9.
The main opinion is that the type of karst water source field and technical conditions of exploiting karst water are different in different environmental conditions.
This paper recorded the Musci of Maolan Karst Forest Area, 186 species (including subspecies and varieties) belong to 93 genera and 28 families are reported.
The main water source is fracture - karst water in Middle Ordovician carbonate rocks.
Epi - Fissure - Karst Zone ( EFKZ ) is commonly observed in karst mountainous area at the middle latitude of P.
What is more, the influence of karst surface of carbonate terrane on red clay formation was analyzed.
The karst fissure medium can be regarded as dual medium of porosity.
Karst cave probing is a very important task in engineering geophysics.
The first is the depression karst development pattern from dissolution of karst hill during Indo-Chinese epoch which is the key period for forming space of the reservoir.