Bell Top Formation | |
---|---|
Stratigraphic range: | |
Type | Formation |
Unit of | Spears Group |
Underlies | Mogollon Group |
Overlies | Palm Park Formation, Datil Group |
Thickness | 800 feet (240 m) |
Lithology | |
Primary | Volcaniclastic |
Location | |
Coordinates | 32°29′47″N 107°07′05″W / 32.4963°N 107.1181°W |
Region | New Mexico |
Country | United States |
Type section | |
Named for | Bell Top Mountain |
Named by | Kottlowski |
Year defined | 1953 |
The Bell Top Formation is a geologic formation in southern New Mexico.[1] Radiometric dating of surrounding tuffs indicate that it was deposited in the Oligocene epoch.[2]