四姑娘山地处青藏高原向四川盆地陡跌的关键区域、中国松潘-甘孜地块与扬子地块的结合部,在独特的古老造山带中孕育了壮美的年轻极高山,完整地记录了青藏高原的隆升过程与机制,其科学和美学性举世瞩目。
        The Mt. Siguniang region is situated in a key location where the Qinghai-Tibet Plateau drops steeply to meet the Sichuan Basin. It also stands at the intersection between Songpan-Ganzi and Yangtze terranes. As the birthplace of a young, beautiful ultra and a museum that perfectly documented the uplift of the Qinghai-Tibet Plateau and the related geological processes, this unique and ancient orogenic belt has captured widespread attention for its aesthetic and scientific value.
       四姑娘山所在的邛崃山脉,群山起伏、冰峰环峙,群峰之下高山峡谷深邃悠长。因处于华西雨屏带边缘,受其气候影响,常年云遮雾绕,为四姑娘高山群峰披上了神秘面纱。
       四姑娘山绝对高度六千多米,从海拔仅数百米的四川盆地边缘拔地而起,极短距离内扶摇直上数千米,快速完成从盆地到高原的地貌切换,极端、悬殊的落差和视觉冲击将四姑娘山奇崛的王后之姿展示得淋漓尽致。