温迪亚山脉(梵文：विन्‍ध्य)是位于印度次大陆中西部的一条地质年龄较老的山脉，它将印度次大陆和分割为北印度（中央平原 (南亚)）和南印度两部分。

温迪亚山脉西起位于古吉拉特半岛东部的古吉拉特邦，靠近该邦与拉贾斯坦邦和中央邦的边界。该山脉向东和向北延伸，横亘了整个印度次大陆，尾端位于默札珀地区，此地靠近恒河流域。由于被该山脉以及更为高耸的阿拉维利山脉阻绝了盛行风，所以山脉以北和以西的土地较为贫瘠荒凉。

该山脉的南麓则是纳尔默达河的发源地，该河沿着温迪亚山脉以及在其南、与之并行的索德布尔岭之间的宽阔峡谷向西汇入阿拉伯海。而在该山脉北麓则产生了数条最终汇入恒河的支流，如加利信德河、巴尔伯蒂河、贝德瓦河和肯河。恒河的另外一条支流——桑河则是起源于温迪亚山脉北麓的东段。

The Vindhya Range (pronounced [ʋɪnd̪ʱyə]) is a complex, discontinuous chain of mountain ridges, hill ranges, highlands and plateau escarpments in west-central India.

Technically, the Vindhyas do not form a single mountain range in the geological sense. The exact extent of the Vindhyas is loosely defined, and historically, the term covered a number of distinct hill systems in central India, including the one that is now known as the Satpura Range. Today, the term principally refers to the escarpment that runs north of and roughly parallel to the Narmada River in Madhya Pradesh, and its hilly extensions. Depending on the definition, the range extends up to Gujarat in the west, and Uttar Pradesh and Bihar in the east.