Flynn Creek crater

Template:Short description Template:Infobox terrestrial impact site Flynn Creek crater is an impact crater situated in Jackson County, Tennessee, approximately 8 km south of Gainesboro.

Description

The impact crater was formed approximately 360 million years ago as a shallow, saucer-shaped crater, Template:Convert in diameter and about Template:Convert deep. A large central hill, highly deformed rim strata, and a breccia lens Template:Convert in thickness were produced during formation. Over Template:Convert of flat lying Middle and Upper Paleozoic limestone and dolomite were brecciated and mixed to a depth of Template:Convert, and at least half of the breccia was ejected from the crater. The remaining breccia contains fragments ranging in size from small grains to megabreccia blocks Template:Convert long. Undisturbed strata lie Template:Convert below the original crater floor.<ref>Template:Cite Earth Impact DB</ref>

In the middle of the crater, a sequence of steeply-dipping, folded, faulted, and brecciated Middle Ordovician limestone and dolomite has been uplifted Template:Convert to form a large central hill. Rock of the Knox group in the central uplift are raised Template:Convert above their normal position and locally contain shatter cones.

In the rim surrounding the crater, Ordovician limestone has been uplifted Template:Convert and is moderately to tightly folded into doubly plunging anticlines and synclines that have axes concentric to the crater walls. In parts of the rim, folds have resulted in radial shortening as great as 35%. Faulting is common in the rim strata and is usually concentric to the crater walls.

In the southeastern rim, a large thrust block forms the crater wall and has been moved out from the crater and uplifted about Template:Convert. The thrust block partly overrides a tilted rim graben that has down-dropped about Template:Convert and moved toward the crater. Overlying this graben is a layer of breccia which is apparently the remains of an ejecta blanket that once surrounded the crater.

Post-crater erosion removed the ejecta, except for the overlying graben, and lowered the regional ground surface less than Template:Convert. Within a few million years of the cratering event the entire structure was covered with shale deposits from the Late Devonian Chattanooga Sea, creating one of the best-preserved ancient impact structures presently known. Subsequent erosion along Flynn Creek drainage has exposed a large extent of the structure. Karst development in the immediate area has created numerous caves associated with impact features, including the only cave known to occur in the central uplift of an impact structure, Hawkins Impact Cave.

Other facts

• ~20 m max pre-impact relief
• ~15 m max depth of water at time of impact
• ~40 m avg breccia thickness
• ~140 m avg breccia depth below crater floor
• ~35% max radial shortening of rim strata
• ~90-190 m range for bolide diameter
• roughly polygonal shape
• lateral zone of disturbance averages 1000 m in extent from crater wall
• lowermost size limit for complex craters with central uplifts
• 1700 m of sediments overlying crystalline basement in area
• conodonts found in immediate crater infill indicate marine environment
• central uplift is composed of strata which have been structurally uplifted 300 m above normal position
• 11.2–72 km/s velocity range for terrestrial impacting bodies
• 25 km/s total vaporization of stony bolides

External links

• United States Geological Survey drilling exploration https://www.usgs.gov/centers/astrogeology-science-center/science/flynn-creek-crater-sample-collection
• Exploration of the Flynn Creek crater