Ripley Formation

603 distinct taxa, from 1,809 fossil occurrences the Paleobiology Database records under this name, spanning 101–66 Mya.

Mississippi, Tennessee, Alabama, Georgia · US

603 taxa · 1,809 fossils · 101–66 Mya

Filed under the Selma Group. Members recorded: Coon Creek Tongue, upper, lower, Keownville, Keownville?, Cuesta, Coon Creek, Cusseta.

Macrostrat places this rock in the Selma Group. Macrostrat’s own record

Ripley Formation — 31.79°N, 85.13°WRipley Formation — 34.73°N, 88.95°WRipley Formation — 34.49°N, 89.01°WRipley Formation — 34.25°N, 90.00°WRipley Formation — 34.93°N, 88.52°WRipley Formation — 35.23°N, 88.61°WRipley Formation — 33.89°N, 89.02°WRipley Formation — 31.92°N, 85.11°WRipley Formation — 34.12°N, 88.88°WRipley Formation — 31.72°N, 85.12°WRipley Formation — 34.60°N, 88.83°WRipley Formation — 32.51°N, 88.01°WRipley Formation — 32.05°N, 86.78°WRipley Formation — 32.13°N, 85.70°WRipley Formation — 34.53°N, 88.90°WRipley Formation — 35.32°N, 88.42°WRipley Formation — 33.43°N, 88.88°WRipley Formation — 35.62°N, 88.12°WRipley Formation — 35.38°N, 88.40°WRipley Formation — 32.22°N, 84.92°WRipley Formation — 35.00°N, 88.60°WRipley Formation — 35.09°N, 88.53°WRipley Formation — 34.56°N, 88.90°WRipley Formation — 34.76°N, 88.91°WRipley Formation — 34.42°N, 88.91°WRipley Formation — 34.93°N, 88.80°WRipley Formation — 34.88°N, 88.73°WRipley Formation — 34.83°N, 88.74°WRipley Formation — 34.17°N, 88.93°WRipley Formation — 32.00°N, 86.57°WRipley Formation — 33.46°N, 88.77°WRipley Formation — 32.06°N, 86.85°WRipley Formation — 32.14°N, 87.29°WRipley Formation — 34.22°N, 89.00°WRipley Formation — 30.90°N, 84.58°WRipley Formation — 33.86°N, 96.83°WRipley Formation — 35.29°N, 88.60°WRipley Formation — 33.53°N, 88.89°WRipley Formation — 33.39°N, 88.74°WRipley Formation — 32.38°N, 84.44°WRipley Formation — 32.67°N, 83.74°WRipley Formation — 31.85°N, 85.15°WRipley Formation — 32.64°N, 88.17°WRipley Formation — 32.15°N, 87.39°WRipley Formation — 36.23°N, 88.20°W

Loading coastlines…

45 distinct localities, where the rock is now rather than where it was laid down. Tectonics draws the world it belonged to.

When

What has been found

The 40 most often recorded, of 603.

What else lived thenRank the rock of a period

Counts are of occurrence records, which measure the rock and the fieldwork together.