西隆高原 Shillong Plateau 印度梅加拉亚邦东部的高原。为一起伏台地，构成梅加拉亚邦的最高部分。高原的西、北、南部陡崖分别称为加罗(Garo)丘陵、贾因蒂亚(Jaintia)丘陵与卡西丘陵。西隆高原为印度半岛高原的外缘，基本由古老岩层组成。有煤、铁、石灰石等矿床，并已开采。最高点西隆峰，耸立西隆城南5公里(3哩)处，海拔1,961公尺(6,433呎)。
西昆仑山前晚新生代地貌与沉积特征记录了西昆仑山及青藏高原西北缘的隆升过程。
The late Cenozoic geomorphologic and sedimentary features in the west Kunlun Mountain front record the uplift process of the west Kunlun Mountains and the western margin of the Qinghai-Tibet Plateau.
位于青藏高原北缘的酒西盆地晚新生代沉积比较敏感和全面记录了高原北部的构造运动和隆升过程。
The sediments of the late Cenozoic in the Jiuxi basin, located in the northern margin of the Tibetan plateau, have sensitively and completely recorded the uplifting process of northern plateau.
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