地势起伏强度 meaning in Chinese
relief intensity
reliefinte ity
Examples
- This dissertation is mainly about regional land resource evaluation and land use analysis based on g1s and soter ( soil and terrain spatial and attribute database ) database . the research content is composed of three parts . the first is medium scale soter database study , in this part , the new landform indexes are studied , which are elevation classification , slope classification and relief index classification
在邯郸地区1 25万soter土壤土地数据库建立方面，主要探讨了适用于该比例尺的主地形体指标，提出海拔高度分组指标、坡度分组指标和地势起伏强度分组指标，并利用上述三个指标组合划分出邯郸地区中坡度丘陵( sh ) 、低坡度山前台地( lm ) 、山谷( lv ) 、中坡度山体( sm ) 、山前倾斜平原( lf )和冲洪积平原( lp ) 6个主地形体组分。 - The unconformability between the loess landform of shaanbei loess plateau and its bedrock shape was pointed out first after the full demonstration . the top of loess formation of the south part in shaanbei is flat which likes " platform " , the shape of the bedrock is rolling that likes ridge , and the bedrock bended to fold . the top of loess formation of the mid - part in shaanbei is rolling , but the shape of the bedrock below begins to get flat , the top of loess formation of the north part in shaanbei , loess mao district , is much more rolling among them , however , its shape of the bedrock below is the flattest relatively likes the platform shape of loess formation in south
具体地讲，陕北高原南部的洛） 11黄土源，黄上层顶部相对平坦，地貌类型以黄土源为主格调，而其下伏基岩地层诏皱相对发育，古地势起伏相对较大：陕北高原中部的延安一安塞黄土梁状（为主）丘陵沟壑区，黄土层顶部起伏相对增大，地貌类型以黄土梁为主格调，而其下伏基岩地层槽皱程度趋弱，地层较平缓，古地势起伏相对降低；陕北高原北部的绥德一子洲黄土赤状（为主）丘陵沟壑区，黄土层顶部起伏度相对最大，地貌类型以黄上赤为主格调，而其下伏基底地层以平缓为特征，古地势起伏强度亦相对较低。