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Riverside Park , Hinds County, Mississippi, USA
| Lat/Long (Decimal) | 32.3339,-90.155 |
|---|---|
| Co-ordinates Derivation | based on nearby landmark |
| Given Location | Mississippi, United States |
| Mindat.org Region (for given coordinates) | Hinds County, Mississippi, USA |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| MHi-1 (Moodys Branch) | Toulmin L. D. (1977) | Moodys Branch | supposedly "Auversian"; stage assignment based on Baum et al. 1994; MHi-1 Moodys Branch=Bartonian (JAS 14 October 2010) | sandstone | 41.3 - 38 Ma Eocene |
| Riverside Park (H-79-11-1) | Elder S. R. (1981) | Moodys Branch | "Late Lutetian - early Priabonian." (T. Hansen, pers. comm.) | siltstone | 47.8 - 33.9 Ma Paleogene |
| Riverside Park (H-79-11-11) | Elder S. R. (1981) | Yazoo Clay | "Late Lutetian - early Priabonian." (T. Hansen, pers. comm.) | "shale" | 47.8 - 33.9 Ma Paleogene |
| Riverside Park (H-79-11-14) | Elder S. R. (1981) | Yazoo Clay | "Late Lutetian - early Priabonian." (T. Hansen, pers. comm.) | "shale" | 47.8 - 33.9 Ma Paleogene |
| Riverside Park (H-79-11-3) | Elder S. R. (1981) | Moodys Branch | "Late Lutetian - early Priabonian." (T. Hansen, pers. comm.) | siltstone | 47.8 - 33.9 Ma Paleogene |
| Riverside Park (H-79-11-6) | Elder S. R. (1981) | Moodys Branch | "Late Lutetian - early Priabonian." (T. Hansen, pers. comm.) | siltstone | 47.8 - 33.9 Ma Paleogene |
| Riverside Park (H-79-11-7) | Elder S. R. (1981) | Moodys Branch | "Late Lutetian - early Priabonian." (T. Hansen, pers. comm.) | siltstone | 47.8 - 33.9 Ma Paleogene |
| Riverside Park (H-79-11-8) | Elder S. R. (1981) | Moodys Branch | "Late Lutetian - early Priabonian." (T. Hansen, pers. comm.) | siltstone | 47.8 - 33.9 Ma Paleogene |
Recorded Fossils
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
