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The Lake Tahoe Watershed (USGS Huc 18100200) of 505 sq mi (1,310 km) includes the land area that drains to the lake and the Lake Tahoe drainage divide traverses the same general area as the Tahoe Rim Trail. These drain an area about the same size as the lake and produce half its water, with the balance entering as rain or snow falling directly on it.

This kind of faulting is characteristic of the geology of the adjoining Great Basin to the east.

Lake Tahoe is the youngest of several extensional basins of the Walker Lane deformation zone that accommodates nearly 12 mm/yr of dextral shear between the Sierra Nevada-Great Valley Block and North America.

Three principal faults form the Lake Tahoe basin: the West Tahoe Fault, aligned between Meyers and Tahoe City, and which is the local segment of the Sierra Nevada Fault, extending on shore north and south of these localities; the Stateline/North Tahoe Fault, starting in the middle of the lake and creating the relief that forms Stateline, NV; and the Incline Village Fault, which runs parallel to the Stateline/North Tahoe Fault offshore and into Incline Village.

The West Tahoe Fault appears to be the most active and potentially hazardous fault in the basin.

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