Picuris Mountains: Difference between revisions
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{{Short description|Mountain range in New Mexico}} |
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{{Infobox mountain range |
{{Infobox mountain range |
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| highest_location = Picuris Peak |
| highest_location = Picuris Peak |
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| range_coordinates = {{coord|36 |
| range_coordinates = {{coord|36|15|N|105|42|W|type:mountain_region:US-NM_dim:20000|display=inline,title}} |
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| map = USA New Mexico |
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The '''Picuris Mountains''' are a mountain range in northern [[New Mexico]]. They are considered a subrange of the [[Sangre de Cristo Mountains]].<ref name="julyan1998"/> |
The '''Picuris Mountains''' are a mountain range in northern [[New Mexico]]. They are considered a subrange of the [[Sangre de Cristo Mountains]].<ref name="julyan1998"/> |
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==Geography== |
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The range resembles a triangle with its base to the east, along the valley of the Rio Grande del Rancho. The northwest face lies along the valley of the [[Rio Grande]] and the southern face lies along Rio Pueblo and [[Embudo |
The mountains are located to the east of [[Dixon, New Mexico|Dixon]] and surround [[Picuris Pueblo, New Mexico|Picuris Pueblo]] to the west, north, and east. The range resembles a triangle with its base to the east, along the valley of the Rio Grande del Rancho. The northwest face lies along the valley of the [[Rio Grande]] and the southern face lies along Rio Pueblo and [[Embudo Creek]]. |
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==History== |
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The area was first visited by Europeans on July 13, 1598, when [[Juan de Oñate]] visited Picuris Pueblo. |
The area was first visited by Europeans on July 13, 1598, when [[Juan de Oñate]] visited Picuris Pueblo. |
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==Geology== |
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The range is underlain by [[Precambrian]] rock beds of the [[Hondo Group]] and [[Vadito Group]].<ref name="jdft2011">{{cite journal |last1=Jones |first1=James V. III |last2=Daniel |first2=Christopher G. |last3=Frei |first3=Dirk |last4=Thrane |first4=Kristine |title=Revised regional correlations and tectonic implications of Paleoproterozoic and Mesoproterozoic metasedimentary rocks in northern New Mexico, USA: New findings from detrital zircon studies of the Hondo Group, Vadito Group, and Marqueñas Formation |journal=Geosphere |date=2011 |volume=7 |issue=4 |pages=974–991 |doi=10.1130/GES00614.1 |url=https://pubs.geoscienceworld.org/geosphere/article-lookup/7/4/974 |access-date=15 April 2020|doi-access=free }}</ref> It is the namesake for the [[Picuris orogeny]]. |
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==Economy== |
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Mining has been historically important in the Picuris Mountains. The [[Harding Pegmatite Mine]] was operated off and on from about 1900 to 1958, when it was donated to the [[University of New Mexico]] as an outdoor geological laboratory. At one time, the mine made New Mexico the leading producer of [[beryllium]] among the United States.<ref name="je1976">{{cite journal |last1=Jahns |first1=Richard H. |last2=Ewing |first2=Rodney C. |title=The Harding Mine Taos County New Mexico |journal=New Mexico Geological Society Field Conference Series |date=1976 |volume=27 |page=263 |url=https://earth315.earth.lsa.umich.edu/Earth_315_Field_Trip_-_New_Mexico/References_files/Jahns76_NWGS_HardingMine.pdf}}</ref> Copper has been mined at Copper Hill north of the Harding Mine. Other commodities historically mined in the range include [[tungsten]], optical [[calcite]], [[bismuth]], and [[aluminosilicates]]. {{As of|2004}}, the MICA mine was the only producer of [[muscovite]] west of the [[Appalachian Mountains]].<ref>{{cite journal |last1=McLemore |first1=V. T. |last2=Mullen |first2=K. E. |year=2004 |title=Mineral resources in Taos County, New Mexico |journal=New Mexico Geological Society Field Conference Series |volume=55 |pages=383-390 |url=https://geoinfo.nmt.edu/staff/mclemore/documents/McLemore_Mullen.pdf |access-date=6 July 2022}}</ref> |
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==See also== |
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{{portal-inline|New Mexico}} |
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==References== |
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[[Category:Mountain ranges of New Mexico]] |
[[Category:Mountain ranges of New Mexico]] |
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Latest revision as of 18:24, 8 December 2023
| Picuris Mountains | |
|---|---|
 Picuris Mountains north of Picuris Pueblo, New Mexico | |
| Highest point | |
| Peak | 10,801 ft (3,292 m), Picuris Peak |
| Dimensions | |
| Length | 15 mi (24 km) east-west |
| Width | 10 mi (16 km) north-south |
| Naming | |
| Etymology | Keres Pee-koo-ree-a, "those who paint"[1] |
| Geography | |
  Picuris Mountains | |
| Country | United States |
| State | New Mexico |
| Range coordinates | 36°15′N 105°42′W / 36.250°N 105.700°W |
The Picuris Mountains are a mountain range in northern New Mexico. They are considered a subrange of the Sangre de Cristo Mountains.[1]
Geography
[edit]The mountains are located to the east of Dixon and surround Picuris Pueblo to the west, north, and east. The range resembles a triangle with its base to the east, along the valley of the Rio Grande del Rancho. The northwest face lies along the valley of the Rio Grande and the southern face lies along Rio Pueblo and Embudo Creek.
History
[edit]The area was first visited by Europeans on July 13, 1598, when Juan de Oñate visited Picuris Pueblo.
Geology
[edit]The range is underlain by Precambrian rock beds of the Hondo Group and Vadito Group.[2] It is the namesake for the Picuris orogeny.
Economy
[edit]Mining has been historically important in the Picuris Mountains. The Harding Pegmatite Mine was operated off and on from about 1900 to 1958, when it was donated to the University of New Mexico as an outdoor geological laboratory. At one time, the mine made New Mexico the leading producer of beryllium among the United States.[3] Copper has been mined at Copper Hill north of the Harding Mine. Other commodities historically mined in the range include tungsten, optical calcite, bismuth, and aluminosilicates. As of 2004[update], the MICA mine was the only producer of muscovite west of the Appalachian Mountains.[4]
See also
[edit]
References
[edit]- ^ a b Julyan, Robert (1998). The Place Names of New Mexico (2 ed.). Albuquerque: University of New Mexico Press. p. 266. ISBN 0-8263-1689-1.
- ^ Jones, James V. III; Daniel, Christopher G.; Frei, Dirk; Thrane, Kristine (2011). "Revised regional correlations and tectonic implications of Paleoproterozoic and Mesoproterozoic metasedimentary rocks in northern New Mexico, USA: New findings from detrital zircon studies of the Hondo Group, Vadito Group, and Marqueñas Formation". Geosphere. 7 (4): 974–991. doi:10.1130/GES00614.1. Retrieved 15 April 2020.
- ^ Jahns, Richard H.; Ewing, Rodney C. (1976). "The Harding Mine Taos County New Mexico" (PDF). New Mexico Geological Society Field Conference Series. 27: 263.
- ^ McLemore, V. T.; Mullen, K. E. (2004). "Mineral resources in Taos County, New Mexico" (PDF). New Mexico Geological Society Field Conference Series. 55: 383–390. Retrieved 6 July 2022.
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