Recent drop in Lake Powell’s storage shows how much space sediment is taking up

Laurine Lassalle/Aspen Journalism
Glen Canyon Dam in Page, Arizona, forms Lake Powell. Bureau data on the reservoir’s water-storage volume showed a loss of 443,000 acre-feet between June 30 and July 1. | Heather Sackett/Aspen Journalism

The Bureau of Reclamation last week revised its data on the amount of water stored in Lake Powell, with a new, lower tally taking into account a 4% drop in the reservoir’s total available capacity between 1986 and 2018 due to sedimentation.

Bureau data on the reservoir’s water-storage volume showed a loss of 443,000 acre-feet between June 30 and July 1 — a 6% drop in storage from 6.87 million acre-feet (which is 28.28% of live storage based on 1986 data) to 6.43 million (26.46% of full).  

The cause was a recalculation of water stored based on a Bureau of Reclamation and U.S.Geological Survey study released in March — the first such analysis in more than 30 years — about Lake Powell’s loss of storage capacity due to the amount of sediment that the Colorado River and other tributaries deposit into the reservoir. The study was based on data about sediment in the lake collected in 2017 and 2018.

“After inputting the new data on July 1, 2022, storage values at the current elevation were updated, resulting in a decrease of 443,000 acre-feet,” bureau officials wrote in an email. 

The Bureau of Reclamation has performed two prior sediment surveys: pre-impoundment (before the construction of the dam — up to 1963) and in 1986. 

Storage capacity figures prior to the release of the report in March had been based on 1986 data, Casey Root, a hydrologist for the U.S. Geological Survey’s Utah Water Science Center, said in an email.

The new data will be included in the upcoming July 24-Month Study, scheduled to be released in mid-July, which forecasts the reservoir’s volume and surface elevation, and in any subsequent operational projections.

Slackwater delta

“Like most reservoirs, Lake Powell loses storage capacity as a result of sedimentation from its source rivers,” said Root, who worked on the most recent USGS and Bureau of Reclamation study.


This animation shows the sedimentation process in Lake Powell. | Courtesy of U.S. Geological Survey

The paper explained that Lake Powell has continuously trapped sediment — including silt, sand and mud — from the Colorado and San Juan rivers since the Glen Canyon Dam impounded the rivers in 1963. The meeting of the free-flowing rivers carrying sediment with the slack water of the reservoir creates a delta, where the sediment falls to the lake’s bottom.

Root explained that the delta regions are located at the furthest extents of Lake Powell and that these areas typically contain the most sediment.

“Sediment isn’t deposited uniformly across the reservoir but rather far from the dam,” he said. “Over time, these deposits can laterally build toward the dam.”

Since it began filling in 1963, the reservoir has lost on average about 33,270 acre-feet in storage capacity each year, according to the study.  

“Lake Powell is unique in that it is a long, narrow, steep-walled canyon, so the deltas have historically been about 150 miles away from Glen Canyon Dam,” Root said. “Simply being far away from the deltas can help buffer the dam and its operations against sedimentation.”

Due to this sedimentation, Lake Powell’s storage capacity at full pool decreased by 6.79% from 1963 to 2018, or a 1.83 million acre-foot loss.

Between 1986 and 2018, it dropped by 4%, which represents a loss of 1.05 million acre-feet in 32 years.

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