JFRCalifornia
Keeper of San Juan Secrets
Everyone on this forum is well aware of how much sedimentation over the years has affected the extent of Lake Powell. It's especially evident as the lake levels fall and reveal things not seen in decades. One of those "things" is vast amounts of sediment, which is pretty dramatically illustrated for anyone who has been to the overlook at Hite, or taken a boat to the end of either the Escalante or San Juan, or even spent time hiking in many of the side canyons of the lake. All that dirt deposited by the rivers feeding Lake Powell has dramatically cut into the extent of the lake. And that will continue.
In the mid-1960s, as the reservoir began to fill, it spread quickly upstream because the gradients in Glen Canyon before the lake were very shallow. By the end of 1963 (when the lake was at about 3400), the lake had already reached White Canyon, and about 20 miles up the San Juan.
As of December 2025, the lake sits at about 3542, the same level as it was in June 1968. However, the extent of the lake is dramatically smaller today than it was then, and it's all because of massive sedimentation that's happened over the decades. The sediment in the vicinity of Hite is well over 100 feet deep.
As part of a side project I'm working on, I put together a few maps to illustrate the change in the lake's extent between June 1968 and December 2025, even though the surface elevation was the same on both dates. It's one thing to read about the changes, but it's more dramatic to see them on a map. In the case of the main stem of the Colorado, the lake extended 30 miles farther (!) in June 1968 than in December 2025; on the San Juan, it was 18 miles. Up the Escalante, the difference is less because of the flow of the Escalante is much less than the big rivers. Still, a 4-mile change is dramatic.
Here are the maps showing the end of the lake along the Colorado, San Juan and the Escalante, comparing June 1968 to December 2025, at the same lake level of 3542...


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In the mid-1960s, as the reservoir began to fill, it spread quickly upstream because the gradients in Glen Canyon before the lake were very shallow. By the end of 1963 (when the lake was at about 3400), the lake had already reached White Canyon, and about 20 miles up the San Juan.
As of December 2025, the lake sits at about 3542, the same level as it was in June 1968. However, the extent of the lake is dramatically smaller today than it was then, and it's all because of massive sedimentation that's happened over the decades. The sediment in the vicinity of Hite is well over 100 feet deep.
As part of a side project I'm working on, I put together a few maps to illustrate the change in the lake's extent between June 1968 and December 2025, even though the surface elevation was the same on both dates. It's one thing to read about the changes, but it's more dramatic to see them on a map. In the case of the main stem of the Colorado, the lake extended 30 miles farther (!) in June 1968 than in December 2025; on the San Juan, it was 18 miles. Up the Escalante, the difference is less because of the flow of the Escalante is much less than the big rivers. Still, a 4-mile change is dramatic.
Here are the maps showing the end of the lake along the Colorado, San Juan and the Escalante, comparing June 1968 to December 2025, at the same lake level of 3542...


..