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Serpent Mound

Precontact effigy mound in Ohio, United States

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Through Clay and Erosion

The first published surveys of the mound, by E. G. Squier and Edwin Hamilton Davis, were featured in their 1848 study Ancient Monuments of the Mississippi Valley, commissioned by the Smithsonian Institution.

The United States Department of the Interior designated the mound as a National Historic Landmark in 1966. It is maintained by the Ohio History Connection, a nonprofit organization dedicated to preserving historical sites in Ohio.

Description

Effigy mounds have been constructed independently by several cultures. The significance of Serpent Mound is based on its size and historical relevance. Made up of three parts, Serpent Mound extends over 1,348 ft (411 m) in length, varying from 9 in (23 cm) to more than 3 ft (91 cm) in height. The mound stands with a width varying between 22 and 24 ft (6.7 and 7.3 m) based on the section. Serpent Mound conforms to the surrounding land, as it was built on a bluff above the Ohio Brush Creek. The mound winds back and forth for more than eight hundred feet, with its tail coiling in seven areas throughout the mound. The mound features a triple-coiled tail at the end of the structure, often viewed as a benchmark of the mound. Yellowish clay and ash make up the main constituents of the mound, with a layer of rocks and soil reinforcing the outer layer.

Squier and Davis interpreted the structure as an open-mouth head of a [serpent] that nearly engulfs an east-facing hollow oval feature and is 120-foot (37 m) long. Squier and Davis believed the oval feature may represent an egg, with an apparent depiction of the snake consuming it. Archaeologist J.P. McLean identified the mound as the body of a frog. The western side of the effigy features a triangular mound approximately 31.6 ft (9.6 m) at its base and long axis. Similar serpent effigies exist in Serpent Mounds Park in Ontario and at Skelmorie in Scotland.

Serpent Mound impact crater

The mound is located on the site of a meteorite impact site known as the Serpent Mound crater. The crater is around 8.7 miles (14 km) in diameter and was formed 252–330 million years ago.

In 2003, the Ohio Department of Natural Resources formed a team of geologists to corroborate the meteorite impact origin of the structure at the Serpent Mound. A previous 1975 survey by S.P. Reidel provided them with a background of information pertaining to the site. This has led archaeologists to believe that the topographic expression of the crater has been completely erased by erosion.

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