A long time ago, there was a giant lake.
It was much bigger than it is now. The lake was very deep and wide. It covered much of the land. Now, we only see small lakes there. Can you find where the big lake was?
A long time ago, there was a giant lake.
It was much bigger than it is now. The weather was cooler and it rained more. This helped the lake grow very large.
The water rose and covered much land. It even reached parts of Idaho and Nevada. Later, the water flowed out in a huge flood. Now, only small lakes like the Great Salt Lake remain. It is fun to imagine that big blue water!
A long time ago, a giant lake covered the West.
We call this Lake Bonneville. It was much bigger than any lake today. It was almost as large as Lake Michigan. The lake was in a closed basin. This means water could not flow out through rivers.
The lake grew because the weather changed. It became cooler. This meant more rain fell. It also meant less water dried up from the sun. About 17,500 years ago, the lake reached its highest level. It even spilled over into Idaho. This spill caused a massive event. We call it the Bonneville flood. A huge amount of water rushed out. It flowed into the Snake River and the Pacific Ocean. This flood made the lake level drop very fast. Today, only small lakes remain in this area. The Great Salt Lake is one of them.
You can still see old shorelines on the mountains. These lines show where the water once sat.
A long time ago, a giant lake filled much of the western United States.
This was Lake Bonneville, a huge body of water from the Late Pleistocene period. It covered most of what we now call western Utah. At its largest, the lake reached into parts of Idaho and Nevada. The lake was so big that it covered almost as much area as modern Lake Michigan. It had a complex shape with many peninsulas and islands.
Today, only smaller lakes like the Great Salt Lake remain in this basin.
This lake worked because of a special balance of water. It lived in a closed basin, meaning no rivers flowed out of it. The water level changed based on how much water came in versus how much left. More rain and snow acted as inputs to fill the lake. Less evaporation from the sun acted as a way to keep the water. When it was cooler, more precipitation fell and less water dried up. This caused the lake to rise and expand across the land.
This process is how the lake grew so large.
Scientists have studied this lake for a very long time. A famous geologist named G.K. Gilbert described its features in 1890. He named the lake after Benjamin Louis Eulalie de Bonneville. This man was a French-born explorer and fur trapper in the American West. While others like Father Escalante saw signs of the old lake, Gilbert's work was monumental. His research helped us understand how the ancient world worked. He set the stage for all the science we do today.
Lake Bonneville had a very busy history with many stages. It began to rise about 30,000 years ago. Around 24,000 years ago, it started to rise very quickly. It reached its highest point about 17,500 years ago. This highest level is known as the Bonneville shoreline. At this time, the water reached the edge of the basin. It eventually spilled over into the Snake River drainage near Red Rock Pass. This overflow created a massive event called the Bonneville flood.
You can still see the history of this lake today. If you look at the mountains near Salt Lake City, you will see shelves. These are the ancient shorelines left behind by the water. They look like benches sticking out from the mountainside. There are three main shorelines named Stansbury, Bonneville, and Provo. These lines show us exactly how high the water once sat. They serve as a map of a world that no longer exists. Even though the lake is gone, its marks remain for us to find.
Lake Bonneville was a massive pluvial lake in western North America. A pluvial lake is a lake that forms because of increased precipitation and decreased evaporation. This lake existed during the Late Pleistocene, a period of major global glaciation. It occupied a hydrographically closed basin, also called an endorheic basin. This means the lake had no river outlets to carry water away.
Today, the Great Salt Lake, Utah Lake, and Sevier Lake are the largest remaining bodies of water in this basin. Lake Bonneville was much larger and deeper than these modern lakes.
The lake's size depended on a specific water balance. This balance is the relationship between water inputs and water outputs. Inputs include precipitation and runoff from rivers. Outputs include evaporation from the lake surface and evapotranspiration from the basin.
When inputs were greater than outputs, the lake level rose. This is called the transgressive phase. When outputs were greater than inputs, the lake level fell. This is called the regressive phase. Changes in global atmospheric circulation drove these climate shifts. These shifts altered the water budget of the entire Great Basin.
Lake Bonneville went through several distinct stages of growth and decline. It began rising about 30,000 years ago from levels similar to the modern Great Salt Lake. During its early transgressive phase, the level fluctuated slightly. Around 24,000 years ago, the lake began a rapid rise to higher elevations. It reached its maximum height about 17,500 years ago. This peak is known as the Bonneville shoreline. At this maximum, the lake covered an area nearly as large as modern Lake Michigan. Its shoreline was complex, featuring many islands and peninsulas.
Scientists identify three main shorelines that can be traced throughout the basin. These are named the Stansbury, Bonneville, and Provo shorelines. The Stansbury and Bonneville shorelines formed during the transgressive phase. The Provo shoreline formed during the overflowing phase. You can see these shorelines today as shelves or benches on mountainsides. They protrude from the mountains above the valley floor. These features are visible from long distances and even on satellite images. They consist of both depositional and erosional segments.
At its highest point, the lake reached the edge of its basin rim. This caused the water to overflow into the Snake River drainage near Red Rock Pass in Idaho. This overflow began as a trickle across a dam formed by the Marsh Creek alluvial fan. Eventually, it became a massive event called the Bonneville flood.
Groundwater sapping on the north slope of the fan made the dam unstable. The dam eventually collapsed, and the flood charged down the Marsh Creek valley. It flowed into the Portneuf River, then the Snake River, and finally the Columbia River. This flood likely lasted less than a year. It caused the lake level to drop by about 100 meters.
The study of Lake Bonneville has a long history. Early explorers noticed the ancient shorelines. Father Silvestre Velez de Escalante saw shell deposits in 1776. Captain John C. Frémont also recognized them in 1843. However, the geologist G.K. Gilbert provided the first major scientific description in 1890. He named the lake after Benjamin Louis Eulalie de Bonneville. Bonneville was a French-born U.S. Army officer and explorer. Gilbert's monumental work set the stage for all modern research on the paleolake.
Understanding Lake Bonneville helps scientists connect local history to global systems. While glaciers were expanding during this time, Lake Bonneville was not a proglacial lake. This means it was not formed directly by melting glaciers. In fact, mountain glaciers in the basin held less than 5% of the lake's maximum water volume. The lake also had no river connection to the massive Laurentide or Cordilleran ice sheets. Instead, the lake was a product of complex atmospheric and climatic changes. This makes it a vital example of how climate drives large-scale environmental shifts.
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