The U.S. Army Corps of Engineers (USACE) built Raystown Dam in 1972 to reduce the risk of flooding to downstream communities by storing water during major flood events. The dam is located on the Raystown Branch Juniata River, approximately 5.5 miles upstream of the confluence with the Juniata River. The dam is located in Huntingdon and Bedford Counties, approximately 3.5 miles south of the Borough of Huntingdon, PA. The dam consists of an earthen embankment, behind which Raystown Lake is impounded. The primary purpose for Raystown Dam is for flood risk management to reduce downstream river levels during flood events. In addition, the water stored in the reservoir and the releases from the dam also provide additional benefits for water quality, hydropower and recreation during non-flood periods. Releases from the dam can be made through the hydropower plant, a gated spillway, and a gated conduit. The project also includes an ungated spillway which can release large flows during extreme flood events. A small earthen embankment named Hesston Dike is also associated with Raystown Dam and is located near the town of Hesston, PA. This dike is listed separately within the National Inventory of Dams and, during large floods, blocks water from flowing out of Raystown Lake at an area of low ground.
What are the risks associated with living near or downstream of Raystown Lake?
Although Raystown Dam reduces the risk of flooding to downstream communities, the dam does not eliminate the risk of flooding. The most likely scenario that could result in downstream flooding from the dam would be a high-volume release of water from the dam’s spillways during significant storm events. To maintain the structural integrity of the dam when the water level in the reservoir gets high, the spillways release water to the Raystown Branch Juniata River. The frequency and amount of water being released could be great enough to cause flooding in downstream communities. Such higher releases from the spillways could create conditions similar to how the river might behave if the dam did not exist.
There are also unlikely, but far more devastating, scenarios involving breach of the dam that would produce significant flooding. This could involve situations such as: a rare, extreme rainfall event resulting in water flowing over the earthen dam, eroding the dam and leading to a breach of the dam; or unexpected behavior of seepage through the dam, eroding soil from within the embankment and leading to a breach of the dam. If a breach were to occur, an uncontrolled surge of water would flow out of the reservoir, flooding downstream communities. Huntingdon, Mapleton, Mt. Union, Lewistown, Shirleysburg, and adjacent communities are in the most immediate danger in the event of a flood. Other communities along the Juniata River would also be impacted.
In any of the scenarios described above, the downstream floodwater would be swift and deep, overflowing levees and destroying buildings and key infrastructure. Those caught unaware and/or unable to evacuate could perish. In the less likely dam breach scenarios, the water depth, property damage, and lives lost would likely be far greater.