Chaco Landscapes White Paper FINAL
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Southwestern Monuments
SOUTHWESTERN MONUMENTS MONTHLY REPORT MAY 1939 UNITED STATES DEPARTMENT OF THE INTERIOR NATIONAL PARK SERVICE GPO W055 UNITED STATES DEPARTMENT OF THE INTERIOR *$*&*">&•• NATIONAL PARK SERVICE / •. •: . • • r. '• WASHINGTON ADDRESS ONLY THE DIRECTOR. NATIONAL PARK SERVICE April 2k. 1939. Memorandum for the Superintendent, Southwestern National Monuments: I am writing this as an open letter to you because all of us recognize the fine friendly spirit engendered by your Southwestern National Monuments n.onthly reports. I believe that all park and monument reports can be made as interesting and informative as yours. Your monthly report for L.erch i6 on my desk and I have glanced through its pages, checking your opening statements, stopping here and there to j.ick up en interesting sidelight, giving a few moments to the supplement, and then looking to your "Ruminations". The month isn't complete unless I read themJ As you know, the submission of the monthly reports from the field has been handled as another required routine statement by some of the field men. It seems to me you have strained every effort to rrake the reports from the Southwestern National Monuments an outstanding re flection of current events, history, and special topics; adding a good share of the personal problems and living conditions of that fine group of men and women that constitute your field organization. You have ac complished a great deal by making the report so interesting that the Custodians look forward to the opportunity of adding their notes. In issuing these new instructions, I am again requesting that the Superintendents and Custodians themselves take the time to put in writing the story of events, conditions, and administration in the parks and monuments they represent. -
Narbonapass.Pdf
FIRST-DAY ROAD LOG 1 FIRST-DAY ROAD LOG, FROM GALLUP TO GAMERCO, YAH-TA-HEY, WINDOW ROCK, FORT DEFIANCE, NAVAJO, TODILTO PARK, CRYSTAL, NARBONA PASS, SHEEP SPRINGS, TOHATCHI AND GALLUP SPENCER G. LUCAS, STEVEN C. SEMKEN, ANDREW B. HECKERT, WILLIAM R. BERGLOF, First-day Road Log GRETCHEN HOFFMAN, BARRY S. KUES, LARRY S. CRUMPLER AND JAYNE C. AUBELE ������ ������ ������ ������� ������ ������ ������ ������ �������� Distance: 141.8 miles ������� Stops: 5 ���� ������ ������ SUMMARY ������ �� ������ �� ����� �� The first day’s trip takes us around the southern �� �� flank of the Defiance uplift, back over it into the �� southwestern San Juan Basin and ends at the Hogback monocline at Gallup. The trip emphasizes Mesozoic— especially Jurassic—stratigraphy and sedimentation in NOTE: Most of this day’s trip will be conducted the Defiance uplift region. We also closely examine within the boundaries of the Navajo (Diné) Nation under Cenozoic volcanism of the Navajo volcanic field. a permit from the Navajo Nation Minerals Department. Stop 1 at Window Rock discusses the Laramide Persons wishing to conduct geological investigations Defiance uplift and introduces Jurassic eolianites near on the Navajo Nation, including stops described in this the preserved southern edge of the Middle-Upper guidebook, must first apply for and receive a permit Jurassic depositional basin. At Todilto Park, Stop 2, from the Navajo Nation Minerals Department, P.O. we examine the type area of the Jurassic Todilto For- Box 1910, Window Rock, Arizona, 86515, 928-871- mation and discuss Todilto deposition and economic 6587. Sample collection on Navajo land is forbidden. geology, a recurrent theme of this field conference. From Todilto Park we move on to the Green Knobs diatreme adjacent to the highway for Stop 3, and then to Stop 4 at the Narbona Pass maar at the crest of the Chuska Mountains. -
Map 3.1 Travel Management Plan
TOADLENA SHEEP SPRINGS GREAT BENDTHE PILLAR 3 NW THE PILLAR 3 NE TANNER LAKE PRETTY ROCKPUEBLO BONITO NW B836108 B636108 B536108 B436108 KIMBETO LYBROOK NW LYBROOK COUNSELORTANCOSA WINDMILL B336108 B236108 B136108 FIVE LAKES CANYON NEREGINA GALLINA ARROYA DEL AGUAYOUNGSVILLE CANONES ABIQUIU Y 134 B836107 B736107 B636107 B536107 B436107 MEDANALES LYDEN VELARDE TRAMPAS PENASCO TRES RITOS CERRO VISTA CHACON W B336107 B136107 B836106 B736106 B636106 B536106 E H B436106 B336106 B236106 B136106 B836105 B736105 B636105 B536105 B436105 B336105 T TOADLENA FIVE LAKES CANYON NW U STA 8 S 6 SONSELA BUTTES B236107 CRYSTAL WASHINGTON PASS S H Y A136109 NASCHITTI CHACO CANYON T W W A836108 THE PILLAR 3 SW A H A736108 THE PILLAR 3 SE Y E A636108 LA VIDA MISSION T T E A436108 PUEBLO BONITO HW 8 A A336108 FIRE ROCK WELL Y 44 ABIQUIU 4 TAOS GREY HILL SPRING T A236108 A836107 LYBROOK SE MULE DAM DEER MESA A636107 TAYLOR RANCH CUBA S A536108 KIN KLIZHIN RUINS A536107 A436107 A336107 NACIMIENTO PEAK JAROSA POLVADERA PEAK SARGENT RANCH A236107 A836106 VALLECITOS CHILI SAN JUAN PUEBLO CHIMAYO TRUCHAS EL VALLE JICARITA PEAK HOLMAN A136108 A736106 A636106 A436106 COMANCHE PEAK A736107 ARROYO CHIJUILLITA A336106 A236106 A136106 A836105 A736105 A636105 A536105 A436105 S A336105 CERRO DEL GRANT 6 A136107 7 T A536106 Y A W T STATE H HWY STAT E E BUELL PARK TODILTO PARK 1 H CHUSKA PEAK 26 W H135109 H835108 EAR ROCK Y H735108 RED LAKE WELL 5 H535108 MILK LAKE NOSE ROCK 18 COYOTE CANYON NW H335108 SEVEN LAKES NEPUEBLO PINTADO STANDING ROCK NW H235108 H135108 STAR LAKE -
Elevated Perespectives.Pdf
E levated perspectives the ultimate time-lapse photography project By Maxine McBrinn 50 El Palacio NE LATE JANUARY MORNING, I WAS research. They were originally stored at the institution’s treated to an aerial overview of the greater headquarters and sometime later were sent to the Labora- Santa Fe region, flying with pilot-photogra- tory of Anthropology. Before 1929 and on through the 1940s, pher Adriel Heisey. His work is featured in Kidder was associated with both the Carnegie Institution and the Museum of Indian Arts and Culture’s the Lab. He served on the Lab’s board and often advised its Oexhibition Oblique Views: Archaeology, Photography, and Time administrators and researchers on a variety of topics. At some alongside images of the northern Southwest and Rio Grande point, Kidder or someone else at the Carnegie Institution created by Charles and Anne Morrow Lindbergh in 1929. must have decided that the Lindberghs’ aerial photos would It was a lovely morning, bright and breezy, the latest snow be most useful in Santa Fe, then as now a center for south- gone from all but the most shadowed spots. As we flew over western archaeology. the Sangre de Cristo mountain range toward Pecos National The Lindberghs’ aerial photographs offer a rare look at the Monument and the archaeological site of Pecos Pueblo, I found condition of the sites, towns, villages, and pueblos as well myself having trouble identifying exactly where we were. as the landscape around them. Not surprisingly, things have Many of my usual, ground-based landscape markers were changed since 1929. -
Apr 3 0 1958 Library
RB5IOHAL GRAVTJIT SURVEY OF THE CARRIZO MOUNTAINS AREA, ARIZONA AHD HEW MEXICO By Donald Plouff APR 3 0 1958 LIBRARY U. S. Geological Survey Released to open file May 8, 1958. 42821 This report has not "been edited or evieved for conformity to Geological Survey standards or nomenclature. Contents Page Abstract - . ».-.-. ... ............... ...... ,-. 3 Introduction -- --- - - .« « -.-.-----«- -.- k Asknovledgments ».« £»- -.» »-. -. « -. -.-...-.»-».»«o. 5 Geology » . - . 5 Gfcrfiral - - ............... «... ... 5 Preeambrian roeks -» . » . .. - 6 IVe-Permian sedimentary rocks «> ----- - .- 9 Permian and younger sedimentary rocks -- « 11 Igneous rocks « 12 Sills and laccoliths > 12 Plugs and dikes - - 13 Structure - - - 15 Field survey - - « - 1? Station location - - 1? Equipment « - ...... - . 17 Elevation control - - - . --. .- .- 18 Gravity measurement - .-- ----- 19 Reduction of data - - - - - 21 Interpretation -« - - 22 References - - -- --- 27 42821 Illustrations Main ref. on Page Figure 1. Index map showing location and structural setting of the Carrizo Mountains area, Arizona and New Mexico -- -- -»- 4 2. Generalized geologic map of the Carrizo Mountains area, Arizona and New Mexico ..» - 6 3- Gravity and geologic profiles along line A-A1 / showing known and inferred intrusives and hypothetical relations at depth - - - . .... 12 k. Dlagramm. trie section of Ship Rock diatreme and *>^ hypothetical extension to depth - - 1J 5. Bouguer gravity anomaly map of the Carrizo Mountains area, Arizona and New Mexico 19 All illustrations are at end of text. Tables Table 1. Generalized section of the sedimentary rocks in the Carrizo Mountains area 10 2. Principal facts for gravity base stations of the Carrizo Mountains area, Arizona and Mexico -- .-* 20 REGIONAL GRAVITY SURVEY1 OF THE CARRIZO MOUNTAINS AREA, ARIZONA AKP KEW MEXICO By Donald Plouff Abstract A total of 570 gravity stations were established within an area of about 1,000 square miles south of the common corner of Colorado, Utah, Arizona, and ffew Mexico. -
The Grants Uranium District, New Mexico: Update on Source, Deposition, and Exploration 1
The Grants Uranium District, New Mexico: Update on Source, Deposition, and Exploration 1 VIRGINIA T. M cLEMORE 2 1. Manuscript received September 2, 2010; Accepted November 28, 2010 2. NM Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, NM, 87801; [email protected] ABSTRACT More than 340 million pounds (lbs) of U 3O8 have been produced from the Grants uranium deposits in New Mexico between 1948 and 2002, and at least 403 million lbs of U 3O8 remain as unmined resources. The Grants district is one of the largest uranium provinces in the world. The Grants district extends from east of Laguna to west of Gallup in the San Juan Basin of New Mexico. Three types of sandstone uranium deposits are recognized: tabular, redistributed (roll-front, fault- related), and remnant-primary. The tabular deposits formed during the Jurassic Westwater Canyon time. Subsequently, oxidizing solutions moved downdip, modifying tabular deposits into redistributed roll- front and fault-related deposits. Evidence, including age dates and geochemistry of the uranium deposits, suggests that redistributed deposits could have been formed shortly after deposition in the early Creta - ceous and from a second oxidation front during the mid-Tertiary. The source of uranium is important in understanding how the Grants deposits formed. Two possible sources exist: 1) the Zuni Mountains, which lie south of the district and consist of a Proterozoic granitic highland enriched in uranium with as much as 11 parts per million, and with high heat flow; and 2) vol - canic rocks erupted from a Jurassic arc volcanism, which formed southwest of the San Juan Basin, and deposited ash over much of the region. -
The Primary Architecture of the Chacoan Culture
9 The Primary Architecture of the Chacoan Culture A Cosmological Expression Anna Sofaer TUDIES BY THE SOLSTICE PROJECT indicate that the solar-and-lunar regional pattern that is symmetri- Smajor buildings of the ancient Chacoan culture cally ordered about Chaco Canyon’s central com- of New Mexico contain solar and lunar cosmology plex of large ceremonial buildings (Sofaer, Sinclair, in three separate articulations: their orientations, and Williams 1987). These findings suggest a cos- internal geometry, and geographic interrelation- mological purpose motivating and directing the ships were developed in relationship to the cycles construction and the orientation, internal geome- of the sun and moon. try, and interrelationships of the primary Chacoan From approximately 900 to 1130, the Chacoan architecture. society, a prehistoric Pueblo culture, constructed This essay presents a synthesis of the results of numerous multistoried buildings and extensive several studies by the Solstice Project between 1984 roads throughout the eighty thousand square kilo- and 1997 and hypotheses about the conceptual meters of the arid San Juan Basin of northwestern and symbolic meaning of the Chacoan astronomi- New Mexico (Cordell 1984; Lekson et al. 1988; cal achievements. For certain details of Solstice Pro- Marshall et al. 1979; Vivian 1990) (Figure 9.1). ject studies, the reader is referred to several earlier Evidence suggests that expressions of the Chacoan published papers.1 culture extended over a region two to four times the size of the San Juan Basin (Fowler and Stein Background 1992; Lekson et al. 1988). Chaco Canyon, where most of the largest buildings were constructed, was The Chacoan buildings were of a huge scale and the center of the culture (Figures 9.2 and 9.3). -
Ancient Maize from Chacoan Great Houses: Where Was It Grown?
Ancient maize from Chacoan great houses: Where was it grown? Larry Benson*†, Linda Cordell‡, Kirk Vincent*, Howard Taylor*, John Stein§, G. Lang Farmer¶, and Kiyoto Futaʈ *U.S. Geological Survey, Boulder, CO 80303; ‡University Museum and ¶Department of Geological Sciences, University of Colorado, Boulder, CO 80309; §Navajo Nation Historic Preservation Department, Chaco Protection Sites Program, P.O. Box 2469, Window Rock, AZ 86515; and ʈU.S. Geological Survey, MS 963, Denver Federal Center, Denver, CO 80225 Edited by Jeremy A. Sabloff, University of Pennsylvania Museum of Archaeology and Anthropology, Philadelphia, PA, and approved August 26, 2003 (received for review August 8, 2003) In this article, we compare chemical (87Sr͞86Sr and elemental) analyses of archaeological maize from dated contexts within Pueblo Bonito, Chaco Canyon, New Mexico, to potential agricul- tural sites on the periphery of the San Juan Basin. The oldest maize analyzed from Pueblo Bonito probably was grown in an area located 80 km to the west at the base of the Chuska Mountains. The youngest maize came from the San Juan or Animas river flood- plains 90 km to the north. This article demonstrates that maize, a dietary staple of southwestern Native Americans, was transported over considerable distances in pre-Columbian times, a finding fundamental to understanding the organization of pre-Columbian southwestern societies. In addition, this article provides support for the hypothesis that major construction events in Chaco Canyon were made possible because maize was brought in to support extra-local labor forces. etween the 9th and 12th centuries anno Domini (A.D.), BChaco Canyon, located near the middle of the high-desert San Juan Basin of north-central New Mexico (Fig. -
Historical Range of Variability and Current Landscape Condition Analysis: South Central Highlands Section, Southwestern Colorado & Northwestern New Mexico
Historical Range of Variability and Current Landscape Condition Analysis: South Central Highlands Section, Southwestern Colorado & Northwestern New Mexico William H. Romme, M. Lisa Floyd, David Hanna with contributions by Elisabeth J. Bartlett, Michele Crist, Dan Green, Henri D. Grissino-Mayer, J. Page Lindsey, Kevin McGarigal, & Jeffery S.Redders Produced by the Colorado Forest Restoration Institute at Colorado State University, and Region 2 of the U.S. Forest Service May 12, 2009 Table of Contents EXECUTIVE SUMMARY … p 5 AUTHORS’ AFFILIATIONS … p 16 ACKNOWLEDGEMENTS … p 16 CHAPTER I. INTRODUCTION A. Objectives and Organization of This Report … p 17 B. Overview of Physical Geography and Vegetation … p 19 C. Climate Variability in Space and Time … p 21 1. Geographic Patterns in Climate 2. Long-Term Variability in Climate D. Reference Conditions: Concept and Application … p 25 1. Historical Range of Variability (HRV) Concept 2. The Reference Period for this Analysis 3. Human Residents and Influences during the Reference Period E. Overview of Integrated Ecosystem Management … p 30 F. Literature Cited … p 34 CHAPTER II. PONDEROSA PINE FORESTS A. Vegetation Structure and Composition … p 39 B. Reference Conditions … p 40 1. Reference Period Fire Regimes 2. Other agents of disturbance 3. Pre-1870 stand structures C. Legacies of Euro-American Settlement and Current Conditions … p 67 1. Logging (“High-Grading”) in the Late 1800s and Early 1900s 2. Excessive Livestock Grazing in the Late 1800s and Early 1900s 3. Fire Exclusion Since the Late 1800s 4. Interactions: Logging, Grazing, Fire, Climate, and the Forests of Today D. Summary … p 83 E. Literature Cited … p 84 CHAPTER III. -
Description of the Telluride Quadrangle
DESCRIPTION OF THE TELLURIDE QUADRANGLE. INTRODUCTION. along the southern base, and agricultural lands water Jura of other parts of Colorado, and follow vents from which the lavas came are unknown, A general statement of the geography, topography, have been found in valley bottoms or on lower ing them comes the Cretaceous section, from the and the lavas themselves have been examined slopes adjacent to the snow-fed streams Economic Dakota to the uppermost coal-bearing member, the only in sufficient degree to show the predominant and geology of the San Juan region of from the mountains. With the devel- imp°rtance- Colorado. Laramie. Below Durango the post-Laramie forma presence of andesites, with other types ranging opment of these resources several towns of tion, made up of eruptive rock debris and known in composition from rhyolite to basalt. Pene The term San Juan region, or simply " the San importance have been established in sheltered as the "Animas beds," rests upon the Laramie, trating the bedded series are several massive Juan," used with variable meaning by early valleys on all sides. Railroads encircle the group and is in turn overlain by the Puerco and higher bodies of often coarsely granular rocks, such as explorers, and naturally with indefinite and penetrate to some of the mining centers of Eocene deposits. gabbro and diorite, and it now seems probable limitation during the period of settle- sa^juan the the interior. Creede, Silverton, Telluride, Ouray, Structurally, the most striking feature in the that the intrusive bodies of diorite-porphyry and ment, is. now quite. -
Annual SF Emmons Lecture Too Warm, Two Poles
Newsletter of the Society May 2017 The objective of the Society is to promote the knowledge and understanding of Earth science, and its application to human needs May Meeting, Thursday, May 18, 2017, 7:00 p.m. American Mountaineering Center Auditorium, 710 10th St., Golden, CO Social time, 6:30; program at 7:00 Annual S.F. Emmons Lecture Too Warm, Two Poles: How Past Super Interglacials Should Inform Future Coastal Policy Julie Brigham-Grette University of Massachusetts, Amherst Glacial and interglacial change uniquely imposed on the Bering Strait region some of the most radical changes in sea level and paleogeography documented in the Northern Hemisphere. Following the transition from a forested Arctic 3 million years ago and the first major glaciation of the northern hemisphere about 2.6 million years ago, marine deposits found along the coasts of Alaska and elsewhere record critical transitions in the evolution of Earth’s climate but especially times of high sea level. Geologic records of Plio-Pleistocene super interglacials from both the Arctic and the Antarctic show us that ice sheets are more vulnerable to subtle polar warming than once thought. Given that sea level rise today and into the near future is global and not reversible, new approaches will require social and political action aimed at short-term fixes and long-term “managed retreat” of human infrastructure from our coastlines. Dr. Julie Brigham-Grette is professor in the Department of Geosciences Climate System Research Center at the University of Massachusetts - Amherst. She graduated from Albion College and completed her M.S. and Ph.D at the University of Colorado, with post-doctoral work at the 1 University of Bergen, Norway, and the University of Alberta, Canada. -
Colorado Topographic Maps, Scale 1:24,000 This List Contains The
Colorado Topographic Maps, scale 1:24,000 This list contains the quadrangle names and publication dates of all Colorado topographic maps published at the scale of 1:24,000 by the U.S. Geological Survey (USGS). One, non-circulating copy of each map is held in the Map Room Office. The Library does not own maps labeled "lacking." The maps are sorted alphabetically by sheet name. Colorado 1:24,000 Topos -- A Abarr 1974 printed 1977 Abarr SE 1968 printed 1971 1968 (without color) printed 1971 Abeyta 1971 printed 1974 1971 (without color) printed 1974 Adams Lake 1974 printed 1978 (dark), 1978 (light) 1974 (without color) printed 1978 1987 printed 1988 Adena 1963 printed 1965, 1975 1963 (without color) printed 1965 1984 printed 1984 1984 (without color) printed 1984 Adler Creek 1968 printed 1971 1968 (without color) printed 1971 Adobe Downs Ranch, New Mexico-Colorado 1963 printed 1965 1963 (without color) printed 1965 1979 printed 1980 (dark), 1980 (light) Adobe Springs 1969 printed 1972, 1992 1969 (without color) printed 1972 Agate 1970 printed 1973 (dark), 1973 (light) 1970 (without color) printed 1973 Agate Mountain 1983 printed 1983 1994 printed 1998 Aguilar 1971 printed 1974 1971 (without color) printed 1974 Akron 1973 printed 1976 1973 (without color) printed 1976 Akron SE 1973 printed 1976 Akron SW 1973 printed 1976 Alamosa East 1966 printed 1968, 1975 1966 (without color) printed 1968 Alamosa West 1966 printed 1969, 1971 1966 (without color) printed 1969 Aldrich Gulch 1957 printed 1958, 1964, 1975 (dark), 1975 (light) 1957 (without color)