BETA TEST - Fossil data and pages are very much experimental and under development. Please report any problems
Bullard-Hunt Quarry I, St. Clair County, Missouri, USA
| Lat/Long (Decimal) | 38.05,-93.7 |
|---|---|
| Co-ordinates Derivation | not explained |
| Given Location | Missouri, United States |
| Mindat.org Region (for given coordinates) | St. Clair County, Missouri, USA |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| Bullard-Hunt Quarry I, Burlington Limestone, Sample 1 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Lower part of Burlington Limestone exposed at this location, although the base of the formation is covered. The top is an erosional surface. Unit 1: 1.1 ft. | dolomite | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry I, Burlington Limestone, Sample 2 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Lower part of Burlington Limestone exposed at this location, although the base of the formation is covered. The top is an erosional surface. Unit 2: 2.2 | dolomite | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry I, Burlington Limestone, Sample 3 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Lower part of Burlington Limestone exposed at this location, although the base of the formation is covered. The top is an erosional surface. Unit 2: 2.2 ft. | dolomite | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry I, Burlington Limestone, Sample 4 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Lower part of Burlington Limestone exposed at this location, although the base of the formation is covered. The top is an erosional surface. Unit 3: 1.4 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry I, Burlington Limestone, Sample 5 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Lower part of Burlington Limestone exposed at this location, although the base of the formation is covered. The top is an erosional surface. Unit 4 = 5.6 ft. | dolomite | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry I, Burlington Limestone, Sample 6 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Lower part of Burlington Limestone exposed at this location, although the base of the formation is covered. The top is an erosional surface. Unit 4 = 5.6 ft. | dolomite | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry I, Burlington Limestone, Sample 7 | Collinson C., Baxter J. W., et al (1981) | Tournaisian | Lower part of Burlington Limestone exposed at this location, although the base of the formation is covered. The top is an erosional surface. Unit 4 = 5.6 ft. | dolomite | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry I, Burlington Limestone, Sample 8 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Lower part of Burlington Limestone exposed at this location, although the base of the formation is covered. The top is an erosional surface. Unit 5: app. 0.5 ft.s | dolomite | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 10 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 7: 18.1 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 11 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 7: 18.1 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 13 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 9: 14.1 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 14 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 9: 14.1 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 15 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 9: 14.1 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 16, 17 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 11 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 18 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 12: 23.3 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 3 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 4: 2.8 ft. | dolomite | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 4 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 4: 2.8 ft. | dolomite | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 5 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 6: 6.9 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 6 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 6: 6.9 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 7 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 7: 18.1 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 8 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 7: 18.1 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Bullard-Hunt Quarry II, Burlington Limestone, Sample 9 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | Upper Part of the Burlington Limestone exposed in this section. Top of outcrop is an erosional surface covered by a Holocene regolith. Lowest bed (Unit 1) correlates to 4 ft below base of Unit 5 in Bullard-Hunt Quarry I section. Unit 7: 18.1 ft. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Osceola North Roadcut, Burlington Limestone, Sample 13 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | This section begins within the Sedalia and proceeds through the North-view, Pierson, and Burlington. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Osceola North Roadcut, Burlington Limestone, Sample 14 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | This section begins within the Sedalia and proceeds through the North-view, Pierson, and Burlington. | dolomite | 358.9 - 346.7 Ma Paleozoic |
| Osceola North Roadcut, Burlington Limestone, Sample 15 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | This section begins within the Sedalia and proceeds through the North-view, Pierson, and Burlington. | dolomite | 358.9 - 346.7 Ma Paleozoic |
| Osceola North Roadcut, Burlington Limestone, Sample 17 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | This section begins within the Sedalia and proceeds through the North-view, Pierson, and Burlington. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
| Osceola North Roadcut, Burlington Limestone, Sample 18 | Collinson C., Baxter J. W., et al (1981) | Burlington Limestone | This section begins within the Sedalia and proceeds through the North-view, Pierson, and Burlington. | "limestone" | 358.9 - 346.7 Ma Paleozoic |
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!
