Plainview (1917) meteorite, Hale Co., Texas, USAi
Regional Level Types | |
---|---|
Plainview (1917) meteorite | Meteorite Fall Location |
Hale Co. | County |
Texas | State |
USA | Country |
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Latitude & Longitude (WGS84):
34° 7' 0'' North , 101° 46' 59'' West
Latitude & Longitude (decimal):
Locality type:
Meteorite Class:
Meteoritical Society Class:
KΓΆppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Hale Center | 2,093 (2017) | 8.1km |
Plainview | 20,919 (2017) | 10.3km |
Seth Ward | 2,025 (2011) | 13.6km |
Edmonson | 105 (2017) | 21.3km |
Kress | 687 (2017) | 27.9km |
Ordinary chondrite, brecciated (H5,br.; S3; W2)
Found, 1917; 700 kg
In 1917 Merrill described in detail 3 meteoritic stones and some fragments (total mass 7.6 kg) which had been found ~8 km SW of Plainview. Merrill was able to provide a moderate inventory of the chondritic mineralogy and an initial description of the thoroughly brecciated textures of what had presumably been a single meteorite breaking up shortly before impact. Despite the strong overlay of its weathering 'varnish,' Merrill further noted regions with distinct color variations (darkening). Several additional stones were received shortly after Merrill prepared his report so that a total of 24 kg had been recovered by the end of 1917. During a two day Plainview stopover in 1933 Harvey Nininger recovered an even larger amount of meteoritic matter. Indeed, over a period of 15 years several 100 kg of additional material were recovered in a ~6 x 26 km strewn field due to his efforts.
As noted by Merrill, the meteorite is dominated by the distinct chondrules (olivine and/or pyroxene-rich), chondrule fragments, matrix, and aggregates of (often weathered) Fe-Ni metal and troilite. Orthopyroxene, clinopyroxene and albitic plagioclase are all present. Using more precise contemporary data, the olivine (Fa~18-19) and low Ca-clinopyroxene (Fs~17) place Plainview (1917) well within the H-chondrite geochemical group. Signs of shock have been explored in detail. Weathering products (goethite, limonite) are also noted by various authors. However, perhaps most significant is that the large mass has allowed a thorough study of minor constituents (Cf., Ramdohr, 1977) as well as some intriguing studies of its exotic clasts.
Plainview (1917)'s cosmic ray exposure (CRE) age of ~6.0 Ma is part of a cluster of 6-10 Ma CRE ages involving more than half of the studied H chondrites with H5 membership especially prominent. Presumably, most of the H5 meteorites which reach the earth during our current epoch were involved in one or two disruptive collisions less than 10 million years ago which then sent numerous small fragments (meteoroids) into eventual collisions with the earth.
The H chondrites (relatively high in total iron) are the second largest group of ordinary chondrites and represent ~40% of the witnessed and fully classified meteorite falls. The H5 petrologic type is the largest H subgroup and accounts for ~50% of the H falls. The Plainview (1917) total mass makes it the 3rd most massive recovered H5 chondrite. Only the 4 ton Jilin, China (1976) and the 1.1 ton Kunya-Urgench, Turkmenistan (1998) H5 falls were more massive.
Specimens of the Plainview (1917) mass have been distributed to a number of institutions worldwide. The largest amount of material is currently held at the Center for Meteorite Studies at Arizona State University (derived from Nininger's holdings). Over 25 kg are also held by the Natural History Museum in London (also mostly derived from Nininger's holdings) and by the United States National Museum in Washington, DC.
What's in a name? For approximately half a century the Plainview (1917) meteorite, an H5 ordinary chondrite, was known simply as the 'Plainview' meteorite. However, in 1950 another 2.2 kg and apparently separate chondritic mass was recovered in the same general area so the two masses were labelled 'Plainview (1917)' and 'Plainview (1950),' respectively. By 2010, three additional chondritic stones had been recovered from nearby, but sometimes somewhat uncertain original sites. In all, 5 separate meteorites are now listed at the Meteoritical Bulletin Database and appear to represent a minimum of at least 3 separate falls. For example, the 'Plainview (d)' meteorite, an L6 chondrite, is clearly a separate fall. The evidence for separate events for the small 'Plainview (c)' and 'Plainview (e)' stones, however, does not appear to be decisive at this time.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
20 valid minerals.
Meteorite/Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
β Augite Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6 Reference: Rubin, A.E., Trigo-Rodriguez, J.M., Kunihiro, T., Kallemeyn, G.W. & Wasson, J.T. (2005) Carbon-rich chondritic clast PV1 from the Plainview H-chondrite regolith breccia: Formation from H3 chondrite material by possible cometary impact. Geochimica et Cosmochimica Acta 69(13): 3419-3430. (July 2005). |
β Chromite Formula: Fe2+Cr3+2O4 Reference: Merrill, G.P. (1917) New find of meteoritic stones near Plainview. Hale County, Texas. Proceedings of the National Museum 52(2184): 419-422,2 plates.; Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages. |
β 'Clinopyroxene Subgroup' Reference: Merrill, G.P. (1917) New find of meteoritic stones near Plainview. Hale County, Texas. Proceedings of the National Museum 52(2184): 419-422,2 plates.; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages. |
β Copper Formula: Cu Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
β Dolomite Formula: CaMg(CO3)2 Reference: Briani et al. (2012) Xenoliths and microliths in H chondrites: Sampling the zodiacal cloud in the asteroid Main Belt. Meteoritics & Planetary Science 47(5): 880-902. (May 2012). |
β 'Fayalite-Forsterite Series' Description: Olivine in host (Fa19.5, Sipiera et al.,1983;Fa17.8, Rubin et al, 2005) w. exotic Olivine in clasts. Reference: Merrill, G.P. (1917) New find of meteoritic stones near Plainview. Hale County, Texas. Proceedings of the National Museum 52(2184): 419-422,2 plates.; Sipiera, S. P., Olsen, E. J., Eatough, D. L., & Dod, B. D. (1983) Summary of several recent chondrite finds from the Texas Panhandle: Meteoritics 18 (1): 63-75. (March 1983).; Rubin, A.E., Trigo-Rodriguez, J.M., Kunihiro, T., Kallemeyn, G.W. & Wasson, J.T. (2005) Carbon-rich chondritic clast PV1 from the Plainview H-chondrite regolith breccia: Formation from H3 chondrite material by possible cometary impact. Geochimica et Cosmochimica Acta 69(13): 3419-3430. (July 2005).; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages. |
β Forsterite Formula: Mg2SiO4 Description: Fayalite content as low as Fa 0.6 and Fa2 reported for various grains. Reference: Rubin, A.E. & Bottke, W.F. (2009) On the origin of shocked CM clasts in H-chondrite regolith breccias: Meteoritics & Planetary Science 44(5): 701-724. (May 2009). |
β 'Glass' Reference: Rubin, A.E., Trigo-Rodriguez, J.M., Kunihiro, T., Kallemeyn, G.W. & Wasson, J.T. (2005) Carbon-rich chondritic clast PV1 from the Plainview H-chondrite regolith breccia: Formation from H3 chondrite material by possible cometary impact. Geochimica et Cosmochimica Acta 69(13): 3419-3430. (July 2005). |
β Goethite Formula: Ξ±-Fe3+O(OH) Description: Terrestrial weathering product often prominent along preexisting veins and cracks. Reference: Rubin, A.E., Trigo-Rodriguez, J.M., Kunihiro, T., Kallemeyn, G.W. & Wasson, J.T. (2005) Carbon-rich chondritic clast PV1 from the Plainview H-chondrite regolith breccia: Formation from H3 chondrite material by possible cometary impact. Geochimica et Cosmochimica Acta 69(13): 3419-3430. (July 2005). |
β Ilmenite Formula: Fe2+TiO3 Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
β Iron Formula: Fe Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
β Iron var. Kamacite Formula: (Fe,Ni) Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
β Isocubanite Formula: CuFe2S3 Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
β 'Limonite' Reference: Rubin, A.E. & Bottke, W.F. (2009) On the origin of shocked CM clasts in H-chondrite regolith breccias: Meteoritics & Planetary Science 44(5): 701-724. (May 2009). |
β Mackinawite Formula: (Fe,Ni)9S8 Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
β Magnesite Formula: MgCO3 Reference: Briani et al. (2012) Xenoliths and microliths in H chondrites: Sampling the zodiacal cloud in the asteroid Main Belt. Meteoritics & Planetary Science 47(5): 880-902. (May 2012). |
β Magnesite var. Breunnerite Formula: (Mg,Fe)CO3 Description: Present in microxenoliths. Reference: Briani et al. (2012) Xenoliths and microliths in H chondrites: Sampling the zodiacal cloud in the asteroid Main Belt. Meteoritics & Planetary Science 47(5): 880-902. (May 2012). |
β Magnetite Formula: Fe2+Fe3+2O4 Reference: Rubin, A.E. & Bottke, W.F. (2009) On the origin of shocked CM clasts in H-chondrite regolith breccias: Meteoritics & Planetary Science 44(5): 701-724. (May 2009).; Briani et al. (2012) Xenoliths and microliths in H chondrites: Sampling the zodiacal cloud in the asteroid Main Belt. Meteoritics & Planetary Science 47(5): 880-902. (May 2012). |
β 'Orthopyroxene Subgroup' Reference: Merrill, G.P. (1917) New find of meteoritic stones near Plainview. Hale County, Texas. Proceedings of the National Museum 52(2184): 419-422,2 plates.; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages. |
β Pentlandite Formula: (NixFey)Ξ£9S8 Reference: Rubin, A.E. & Bottke, W.F. (2009) On the origin of shocked CM clasts in H-chondrite regolith breccias: Meteoritics & Planetary Science 44(5): 701-724. (May 2009).; Briani et al. (2012) Xenoliths and microliths in H chondrites: Sampling the zodiacal cloud in the asteroid Main Belt. Meteoritics & Planetary Science 47(5): 880-902. (May 2012). |
β Perovskite Formula: CaTiO3 Reference: Rubin, A.E. & Bottke, W.F. (2009) On the origin of shocked CM clasts in H-chondrite regolith breccias: Meteoritics & Planetary Science 44(5): 701-724. (May 2009). |
β Pigeonite Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6 Reference: Rubin, A.E., Trigo-Rodriguez, J.M., Kunihiro, T., Kallemeyn, G.W. & Wasson, J.T. (2005) Carbon-rich chondritic clast PV1 from the Plainview H-chondrite regolith breccia: Formation from H3 chondrite material by possible cometary impact. Geochimica et Cosmochimica Acta 69(13): 3419-3430. (July 2005). |
β 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 Description: Plagioclase composition (oligoclase)- An 18.8Ab75.0Or6.2. Reference: Sipiera, S. P., Olsen, E. J., Eatough, D. L., & Dod, B. D. (1983) Summary of several recent chondrite finds from the Texas Panhandle: Meteoritics 18 (1): 63-75. (March 1983).; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages. |
β 'Plessite' Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
β 'Pyroxene Group' Formula: ADSi2O6 Description: Several pyroxenes are present (pigeonite, augite, 'bronzite' and 'clinobronzite' as well as rare grains of either enstatite or clinoenstatite sensu strictu (Fs<10). Reference: Rubin, A.E., Trigo-Rodriguez, J.M., Kunihiro, T., Kallemeyn, G.W. & Wasson, J.T. (2005) Carbon-rich chondritic clast PV1 from the Plainview H-chondrite regolith breccia: Formation from H3 chondrite material by possible cometary impact. Geochimica et Cosmochimica Acta 69(13): 3419-3430. (July 2005). |
β Pyrrhotite Formula: Fe1-xS Description: Pyrrhotite is the dominant sulfide in a hydrated CM clast. Reference: Rubin, A.E. & Bottke, W.F. (2009) On the origin of shocked CM clasts in H-chondrite regolith breccias: Meteoritics & Planetary Science 44(5): 701-724. (May 2009).; Briani et al. (2012) Xenoliths and microliths in H chondrites: Sampling the zodiacal cloud in the asteroid Main Belt. Meteoritics & Planetary Science 47(5): 880-902. (May 2012). |
β Schreibersite Formula: (Fe,Ni)3P Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages. |
β Spinel Formula: MgAl2O4 Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.; Rubin, A.E. & Bottke, W.F. (2009) On the origin of shocked CM clasts in H-chondrite regolith breccias: Meteoritics & Planetary Science 44(5): 701-724. (May 2009). |
β Taenite Formula: (Fe,Ni) Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.; Rubin, A.E., Trigo-Rodriguez, J.M., Kunihiro, T., Kallemeyn, G.W. & Wasson, J.T. (2005) Carbon-rich chondritic clast PV1 from the Plainview H-chondrite regolith breccia: Formation from H3 chondrite material by possible cometary impact. Geochimica et Cosmochimica Acta 69(13): 3419-3430. (July 2005). |
β Troilite Formula: FeS Reference: Merrill, G.P. (1917) New find of meteoritic stones near Plainview. Hale County, Texas. Proceedings of the National Museum 52(2184): 419-422,2 plates.; Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.; Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages. |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
β | Copper | 1.AA.05 | Cu |
β | Iron | 1.AE.05 | Fe |
β | var. Kamacite | 1.AE.05 | (Fe,Ni) |
β | Schreibersite | 1.BD.05 | (Fe,Ni)3P |
β | Taenite | 1.AE.10 | (Fe,Ni) |
Group 2 - Sulphides and Sulfosalts | |||
β | Isocubanite | 2.CB.55b | CuFe2S3 |
β | Mackinawite | 2.CC.25 | (Fe,Ni)9S8 |
β | Pentlandite | 2.BB.15 | (NixFey)Ξ£9S8 |
β | Pyrrhotite | 2.CC.10 | Fe1-xS |
β | Troilite | 2.CC.10 | FeS |
Group 4 - Oxides and Hydroxides | |||
β | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
β | Goethite | 4.00. | Ξ±-Fe3+O(OH) |
β | Ilmenite | 4.CB.05 | Fe2+TiO3 |
β | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
β | Perovskite | 4.CC.30 | CaTiO3 |
β | Spinel | 4.BB.05 | MgAl2O4 |
Group 5 - Nitrates and Carbonates | |||
β | Dolomite | 5.AB.10 | CaMg(CO3)2 |
β | Magnesite | 5.AB.05 | MgCO3 |
β | var. Breunnerite | 5.AB.05 | (Mg,Fe)CO3 |
Group 9 - Silicates | |||
β | Augite | 9.DA.15 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
β | Forsterite | 9.AC.05 | Mg2SiO4 |
β | Pigeonite | 9.DA.10 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Unclassified Minerals, Rocks, etc. | |||
β | 'Clinopyroxene Subgroup' | - | |
β | 'Fayalite-Forsterite Series' | - | |
β | 'Glass' | - | |
β | 'Limonite' | - | |
β | 'Orthopyroxene Subgroup' | - | |
β | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
β | 'Plessite' | - | |
β | 'Pyroxene Group' | - | ADSi2O6 |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | β Goethite | Ξ±-Fe3+O(OH) |
C | Carbon | |
C | β Magnesite var. Breunnerite | (Mg,Fe)CO3 |
C | β Dolomite | CaMg(CO3)2 |
C | β Magnesite | MgCO3 |
O | Oxygen | |
O | β Chromite | Fe2+Cr23+O4 |
O | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
O | β Ilmenite | Fe2+TiO3 |
O | β Spinel | MgAl2O4 |
O | β Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
O | β Pyroxene Group | ADSi2O6 |
O | β Goethite | Ξ±-Fe3+O(OH) |
O | β Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
O | β Forsterite | Mg2SiO4 |
O | β Magnetite | Fe2+Fe23+O4 |
O | β Perovskite | CaTiO3 |
O | β Magnesite var. Breunnerite | (Mg,Fe)CO3 |
O | β Dolomite | CaMg(CO3)2 |
O | β Magnesite | MgCO3 |
Na | Sodium | |
Na | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Mg | Magnesium | |
Mg | β Spinel | MgAl2O4 |
Mg | β Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Mg | β Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Mg | β Forsterite | Mg2SiO4 |
Mg | β Magnesite var. Breunnerite | (Mg,Fe)CO3 |
Mg | β Dolomite | CaMg(CO3)2 |
Mg | β Magnesite | MgCO3 |
Al | Aluminium | |
Al | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Al | β Spinel | MgAl2O4 |
Si | Silicon | |
Si | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Si | β Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Si | β Pyroxene Group | ADSi2O6 |
Si | β Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Si | β Forsterite | Mg2SiO4 |
P | Phosphorus | |
P | β Schreibersite | (Fe,Ni)3P |
S | Sulfur | |
S | β Troilite | FeS |
S | β Isocubanite | CuFe2S3 |
S | β Mackinawite | (Fe,Ni)9S8 |
S | β Pyrrhotite | Fe1-xS |
S | β Pentlandite | (NixFey)Ξ£9S8 |
Ca | Calcium | |
Ca | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Ca | β Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Ca | β Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Ca | β Perovskite | CaTiO3 |
Ca | β Dolomite | CaMg(CO3)2 |
Ti | Titanium | |
Ti | β Ilmenite | Fe2+TiO3 |
Ti | β Perovskite | CaTiO3 |
Cr | Chromium | |
Cr | β Chromite | Fe2+Cr23+O4 |
Fe | Iron | |
Fe | β Chromite | Fe2+Cr23+O4 |
Fe | β Troilite | FeS |
Fe | β Ilmenite | Fe2+TiO3 |
Fe | β Isocubanite | CuFe2S3 |
Fe | β Iron var. Kamacite | (Fe,Ni) |
Fe | β Mackinawite | (Fe,Ni)9S8 |
Fe | β Schreibersite | (Fe,Ni)3P |
Fe | β Taenite | (Fe,Ni) |
Fe | β Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Fe | β Goethite | Ξ±-Fe3+O(OH) |
Fe | β Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
Fe | β Magnetite | Fe2+Fe23+O4 |
Fe | β Pyrrhotite | Fe1-xS |
Fe | β Pentlandite | (NixFey)Ξ£9S8 |
Fe | β Iron | Fe |
Fe | β Magnesite var. Breunnerite | (Mg,Fe)CO3 |
Ni | Nickel | |
Ni | β Iron var. Kamacite | (Fe,Ni) |
Ni | β Mackinawite | (Fe,Ni)9S8 |
Ni | β Schreibersite | (Fe,Ni)3P |
Ni | β Taenite | (Fe,Ni) |
Ni | β Pentlandite | (NixFey)Ξ£9S8 |
Cu | Copper | |
Cu | β Copper | Cu |
Cu | β Isocubanite | CuFe2S3 |
References
Sort by
Year (asc) Year (desc) Author (A-Z) Author (Z-A)Merrill, G.P. (1917) New find of meteoritic stones near Plainview. Hale County, Texas. Proceedings of the National Museum 52(2184): 419-422,2 plates.
Nininger, H.H. (1972). Find a Falling Star. Paul S. Eriksson, Inc.: New York. 254 pages.
Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
Sipiera, S. P., Olsen, E. J., Eatough, D. L., & Dod, B. D. (1983) Summary of several recent chondrite finds from the Texas Panhandle: Meteoritics 18 (1): 63-75. (March 1983).
Grady, M.M (2000). Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pages.
Rubin, A.E., Trigo-Rodriguez, J.M., Kunihiro, T., Kallemeyn, G.W. & Wasson, J.T. (2005) Carbon-rich chondritic clast PV1 from the Plainview H-chondrite regolith breccia: Formation from H3 chondrite material by possible cometary impact. Geochimica et Cosmochimica Acta 69(13): 3419-3430. (July 2005).
Rubin, A.E. & Bottke, W.F. (2009) On the origin of shocked CM clasts in H-chondrite regolith breccias: Meteoritics & Planetary Science 44(5): 701-724. (May 2009).
Briani et al. (2012) Xenoliths and microliths in H chondrites: Sampling the zodiacal cloud in the asteroid Main Belt. Meteoritics & Planetary Science 47(5): 880-902. (May 2012).
Grady, M.M., Pratesi, G. & Moggi-Cecchi, V. (2015) Atlas of Meteorites. Cambridge University Press: Cambridge, United Kingdom. 373 pages.
External Links
http://www.lpi.usra.edu/meteor/metbull.php - MeteoriticalBulletinDatabase
http://www.lpi.usra.edu/meteor/metbull.php?code=18841 -Plainview (1917)@MetBullDatabase
http://www.lpi.usra.edu/meteor/get_original_photo.php?recno=5631513 -Plainview fragment (photo)
http://meteoritegallery.com/wp-content/uploads/2014/04/USNMP-52_2184_1917.pdf -Plainview@Merrill(1917)
http://www.lpi.usra.edu/meteor/metbull.php?code=18841 -Plainview (1917)@MetBullDatabase
http://www.lpi.usra.edu/meteor/get_original_photo.php?recno=5631513 -Plainview fragment (photo)
http://meteoritegallery.com/wp-content/uploads/2014/04/USNMP-52_2184_1917.pdf -Plainview@Merrill(1917)
Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Palo Duro BasinBasin
- Shawnee DomainDomain
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Plainview (1917) meteorite, Hale Co., Texas, USA