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Ferguson Hill section, Mineral County, Nevada, USA
Lat/Long (Decimal) | 38.487,-118.083 |
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Co-ordinates Derivation | estimated from map |
Given Location | Nevada, United States |
Mindat.org Region (for given coordinates) | Mineral County, Nevada, USA |
Collections
Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
---|---|---|---|---|---|
Ferguson Hill section, Unit 106, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Muller Canyon | upper part of Muller Canyon member; unit 106 (total thickness: 26cm) | wackestone | 201.3 - 196.5 Ma Early Jurassic |
Ferguson Hill section, Unit 108, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Muller Canyon | upper part of Muller Canyon member; unit 108 (total thickness: 30cm) | wackestone | 201.3 - 196.5 Ma Early Jurassic |
Ferguson Hill section, Unit 110, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Sunrise - Ferguson Hill | lowermost Ferguson Hill member; unit 110 (total thickness approx. 80cm) | packstone | 201.3 - 196.5 Ma Early Jurassic |
Ferguson Hill section, Unit 94 (uppermost), New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Muller Canyon | middle part of Muller Canyon member; unit 94 (total thickness: 380cm, material collected from uppermost part of unit); proposed level for base of Jurassic. Spelae zone predates European Planorbis zone sensu stricto, but Planorbis is used as an equivalent to Early Hettangian here. | siltstone | 201.3 - 196.5 Ma Early Jurassic |
Ferguson Hill section, Unit 95, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Muller Canyon | middle part of Muller Canyon member; unit 95 (total thickness: 60cm). Spelae zone predates European Planorbis zone sensu stricto, but Planorbis is used as an equivalent to Early Hettangian here. | "limestone" | 201.3 - 196.5 Ma Early Jurassic |
Ferguson Hill section, Unit 96, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Muller Canyon | middle part of Muller Canyon member; unit 96 (total thickness: 280cm). Spelae zone predates European Planorbis zone sensu stricto, but Planorbis is used as an equivalent to Early Hettangian here. | siltstone | 201.3 - 196.5 Ma Early Jurassic |
Ferguson Hill section, Units 100-101, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Muller Canyon | upper part of Muller Canyon member; units 100-101 (total thickness: 40cm). Spelae zone predates European Planorbis zone sensu stricto, but Planorbis is used as an equivalent to Early Hettangian here. | lime mudstone | 201.3 - 196.5 Ma Early Jurassic |
Ferguson Hill section, Units 103-104, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Muller Canyon | upper part of Muller Canyon member; units 103-104 (total thickness: 17cm). Spelae zone predates European Planorbis zone sensu stricto, but Planorbis is used as an equivalent to Early Hettangian here. | wackestone | 201.3 - 196.5 Ma Early Jurassic |
Ferguson Hill section, Units 97-98, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Muller Canyon | upper part of Muller Canyon member; units 97-98 (total thickness: 34cm). Spelae zone predates European Planorbis zone sensu stricto, but Planorbis is used as an equivalent to Early Hettangian here. | "limestone" | 201.3 - 196.5 Ma Early Jurassic |
Ferguson Hill, section e, bed 28 | Taylor D. G., Guex J. (2002) | Gabbs - Muller Canyon | The Spelae zone precedes the true Planorbis zone, but "Planorbis" is used in the sense of Early Hettangian here. | "limestone" | 201.3 - 196.5 Ma Early Jurassic |
Ferguson Hill, section e, bed 90 | Taylor D. G., Guex J. (2002) | Sunrise - Ferguson Hill | "limestone" | 201.3 - 196.5 Ma Early Jurassic | |
Ferguson Hill section, Unit 85, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Mount Hyatt | upper part of Mount Hyatt member; latest Rhaetian; unit 85 (total thickness: 83cm) | "limestone" | 208.5 - 201.3 Ma Mesozoic |
Ferguson Hill section, Unit 86, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Mount Hyatt | upper part of Mount Hyatt member; latest Rhaetian; unit 86 (total thickness: 70cm) | siltstone | 208.5 - 201.3 Ma Mesozoic |
Ferguson Hill section, Unit 88, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Muller Canyon | lower part of Muller Canyon member; latest Rhaetian; unit 88 (total thickness: 30cm) | "limestone" | 208.5 - 201.3 Ma Mesozoic |
Ferguson Hill section, Unit 89, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Muller Canyon | lower part of Muller Canyon member; latest Rhaetian; unit 89 (total thickness: 40cm) | siltstone | 208.5 - 201.3 Ma Mesozoic |
Ferguson Hill section, Unit 90, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Muller Canyon | lower part of Muller Canyon member; latest Rhaetian; unit 90 (total thickness: 140cm) | siltstone | 208.5 - 201.3 Ma Mesozoic |
Ferguson Hill section, Unit 93, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Muller Canyon | lower part of Muller Canyon member; latest Rhaetian; unit 93 (total thickness: 30cm) | "limestone" | 208.5 - 201.3 Ma Mesozoic |
Ferguson Hill section, Units 81-83, New York Canyon area | Lucas S. G., Taylor D. G., et al (2007) | Gabbs - Mount Hyatt | upper part of Mount Hyatt member; latest Rhaetian; units 81-83 (total thickness: 46cm) | "siliciclastic" | 208.5 - 201.3 Ma Mesozoic |
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!