FCPP and Navajo Mine Energy Project, Final
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												  Origin of Non-Bedded Pyroclastic Rocks in the Cathedral Cliff Diatreme, Navajo Volcanic Field, New MexicoThe following document is a pre-print version of: Bélanger C, Ross P-S (2018) Origin of nonbedded pyroclastic rocks in the Cathedral Cliff diatreme, Navajo volcanic field, New Mexico. Bull. Volc. 80:article 61, DOI 10.1007/s00445-018-1234-0 Origin of non-bedded pyroclastic rocks in the Cathedral Cliff diatreme, Navajo volcanic field, New Mexico Caroline Bélanger*, Pierre-Simon Ross Institut national de la recherche scientifique, 490 rue de la Couronne, Québec (Qc), G1K 9A9, Canada * Corresponding author. E-mail addresses: [email protected] (C. Bélanger), [email protected] (P.-S. Ross) Keywords : Diatreme, non-bedded pyroclastic rocks, phreatomagmatic, Navajo volcanic field Abstract Cathedral Cliff is a well exposed mid-Tertiary phreatomagmatic diatreme in the Navajo volcanic field, New Mexico. Post-eruptive erosion, estimated between 500 m and 1000 m, exposes the deep part of the diatreme. Cathedral Cliff provides an opportunity to examine the transition between the bedded pyroclastic rocks of an upper diatreme, and the non-bedded pyroclastic rocks of the subjacent lower diatreme. Bedded pyroclastic rocks occupy 49% of the mapped diatreme area, non-bedded pyroclastic rocks occupy 45%, and the remaining 6% consists of sedimentary megablocks. The bedded pyroclastic rocks range from coarse tuff to medium lapilli tuff, and from lithic to juvenile rich. They were emplaced during eruption at the bottom of the crater by pyroclastic density currents, pyroclastic fallout, and as ballistic bombs and blocks. As the eruption continued, they subsided into the diatreme to their current location. Bedding ranges from well-preserved (“continuous beds”) to partially destroyed (“broken beds”).
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												  Volcanologie Du Diatrème De Cathedral Cliff, Champ Volcanique Navajo, Nouveau-MexiqueUniversité du Québec Institut National de la Recherche Scientifique Centre Eau Terre Environnement VOLCANOLOGIE DU DIATRÈME DE CATHEDRAL CLIFF, CHAMP VOLCANIQUE NAVAJO, NOUVEAU-MEXIQUE Par Caroline Bélanger Mémoire présenté pour l’obtention du grade de Maître ès sciences (M.Sc.) en Sciences de la Terre Jury d’évaluation Examinateur externe John Stix Université McGill Examinateur interne et Michel Malo président du jury INRS Centre Eau Terre Environnement Directeur de recherche Pierre-Simon Ross INRS Centre Eau Terre Environnement © Droits réservés de Caroline Bélanger, 2017 ii RÉSUMÉ Les maars-diatrèmes sont des volcans subaériens caractéristiques des champs volcaniques continentaux monogénétiques ayant des compositions ultramafiques à felsiques. Ces volcans sont le résultat d’éruptions phréatomagmatiques provenant de l’interaction explosive entre le magma et de l’eau souterraine ou entre le magma et des sédiments saturés en eau. La majorité des études portant sur les maars-diatrèmes décrivent le cratère et l’anneau pyroclastique qui l’entoure, fournissant seulement de l’information sur une partie des processus volcaniques ayant lieu dans le diatrème, car plusieurs explosions n’éjectent pas du matériel jusqu’à l’atmosphère. L’étude de diatrèmes est alors nécessaire pour bien comprendre les différents processus volcaniques ayant lieu plus en profondeur. Ce projet de maîtrise porte sur Cathedral Cliff, un diatrème Tertiaire exposé dans le champ volcanique Navajo, au Nouveau-Mexique. Une érosion post-éruptive estimée entre 500 m et 1000 m permet d’exposer la partie plus profonde du diatrème. Cathedral Cliff offre une opportunité d’étudier la transition entre les dépôts pyroclastiques lités, du diatrème supérieur, et les dépôts pyroclastiques non-lités, du diatrème inférieur.
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												  Geochemical Study of Xenoliths from the Navajo- - - - - - • Geochemical study of xenoliths from the  Navajo Volcanic Field; - Arizona, New Mexico, and Utah - .. -.. -.. ..- - by • Patrick D. Mattie - .. - -- • - A Thesis Submitted in Partial Fulfillment of the Requirements for Master of Science in Geochemistry - November, 1996 .. - .. New Mexico Institute of Mining and Technology .. - Socorro, New Mexico, USA - - - Abstract - The Navajo Volcanic Field offers a unique area to study mafic xenoliths due to an - abundance of dikes and diatremes with associated crustal xenoliths. Mafic xenoliths in - kimberlite pipes and minette diatremes in the Navajo Volcanic Field are of four - lithologic types, in order of decreasing abundance: garnet granulite, amphibolite, - pyroxene granulite, and gabbro. Mafic xenoliths from 3 kimberlites and 3 minettes - define eight geochemical groups, of which Groups I and III occur only in Moses Rock dike - (gabbros) and Red Mesa pipe (amphibolites), respectively. With these two exceptions, - there is no correlation of chemical groups with xenolith or host-rock lithology, - geographic location, or degree of xenolith alteration or metamorphism. - - Group I (n=8) with high Mg numbers (0.7-0.8) and high CaO/Ti02(20-60) and low - Ti02 «0.5wt%), shows only slight chondrite-normalized LREE enrichment, and a strong subduction zone component (SZC) (depletion in Nb and Ta relative to neighboring - incompatible elements) and positive Sr, Ba, Eu, and K (SBEK) anomalies on primitive - mantle normalized spidergrams. Group II (n=5) with intermediate CaO/Ti02 (10-20) and Ti02 (0.5-0.9 wt%) has flat to LREE depleted patterns, a SZC and SBEK anomalies. - Group III (n=3) with very high CaO/Ti02 (40-60) and low Ti02 « 0.5 wt%) has nearly flat REE patterns, a very prominent SZC and large SBEK anomalies.
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												  FCPP and Navajo Mine Energy Project, FinalFour Corners Power Plant and Navajo Mine Energy Project Final Environmental Impact Statement 4.16 Recreation Recreational resources for the purposes of this EIS are generally defined as recreational activities such as wildlife viewing, hunting, fishing, picnicking, hiking, and sightseeing, and the publicly accessible facilities and land areas that provide these recreational opportunities. The primary ROI examined for recreational resources encompasses the ROI associated with the Navajo Mine, which includes the Navajo Mine and Pinabete SMCRA Permit Areas, the FCPP, and the ROWs associated with the four transmission lines (see Section 1.1). In addition, the ROI includes regional recreational resources within the Four Corners region generally within 15 to 20 miles of the Navajo Mine and FCPP and approximately 5 miles from the transmission line ROWs. The regional recreational resources ROI is the general viewing area in which the Project features and activities could indirectly affect recreational opportunities and experiences. This ROI is consistent with the BLM’s VRM Process (BLM 2012b), which defines distant or seldom seen views at greater than 15 miles from the proposed activities (see also Section 4.13, Visual Resources). 4.16.1 Regulatory Compliance Framework 4.16.1.1 Navajo Nation Recreation Management The Navajo Nation requires permits for all recreation-related activities on the Navajo Nation tribal trust lands. The Navajo Parks and Recreation Department issues camping, hiking, or backcountry permits (Navajo Nation Parks and Recreation 2012a). Hunting and fishing permits are issued by the NNDFW. The area within 10 miles of the Pinabete SMCRA Permit Area and the FCPP is within Navajo Nation Hunting Unit 13, which is managed for archery, muzzleloader, and rifle deer and elk hunts (NNDFW 2012a).