Paleomap
![Lake-Bonneville-and-Utah.jpeg](https://brightspotcdn.byu.edu/dims4/default/c6ea776/2147483647/strip/true/crop/364x431+0+0/resize/364x431!/quality/90/?url=https%3A%2F%2Fbrigham-young-brightspot.s3.amazonaws.com%2Fa0%2Fa6%2Fc7b579c44d3490f3ef5a069d9b75%2Flake-bonneville-and-utah.jpeg)
At its highest level, 14,500 years ago, Lake Bonneville covered over 40% of the state of Utah. Most valleys in Utah, below 5090 feet in elevation, were filled with the waters of this large freshwater lake. (Illustration by USDA)
![Pleisocene-Lakes.jpeg](https://brightspotcdn.byu.edu/dims4/default/4df0c08/2147483647/strip/true/crop/400x525+0+0/resize/400x525!/quality/90/?url=https%3A%2F%2Fbrigham-young-brightspot.s3.amazonaws.com%2F1f%2Ffd%2F3bef09994214b8f849ac646e2e4e%2Fpleisocene-lakes.jpeg)
On a larger scale, Lake Bonneville was part of a system of freshwater lakes that filled valleys across Nevada, California, and Oregon during the Pleistocene Epoch.
To view, a close-up of Utah Valley and Lake Bonneville click here.
(Image by Ken Perry, Chalk Butte Inc.)