Introduction What Is the Underdark Like?
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Nancy Hultgren Remembers.Pdf
PART III: Carlsbad Caverns National Park, New Mexico The “main focus” of our five-day trip, in the early spring of 1952, was extended time to visit two locations—Carlsbad Caverns National Park, in the southeastern part of the State of New Mexico, and Ciudad Juarez, Mexico—across the International Border from El Paso, Texas, which lies in the far western tip of Texas. A beautiful morning awaited as we rose from our beds in the small motel in the town of Carlsbad, New Mexico. Out in the parking lot, in front of our room, the Hudson was covered with a thick layer of dust, accumulated during our long drive through Colorado and New Mexico. No rain in sight to help wash the car off, but my dad pulled into a Texaco Gas Station in town to refuel, and have the attendant check the oil and clean the windshields and side windows for us. (While living in Denver, Colorado, my dad often frequented a favorite Texaco Station on Colorado Blvd., not far from our first house on Birch Street.) In a friendly tone, and looking at our license plates, which read “Colorful Colorado,” the station attendant asked, “How far have you folks come? Headed for the Caverns I bet! Any time of year is a good time to go, ya’ know! Doesn’t matter what the temperature is on the outside today, cause deep in the Caverns the temperature is the same year round—56°.” Motel Stevens in Carlsbad, New Mexico. Curt Teich vintage linen postcard. Leaving Carlsbad and the Pecos River Valley behind, my dad pointed the Hudson southwest out of town on US Hwy. -
2015 Visitor Guide Park Information and Maps
National Park Service Wind Cave National Park U.S. Department of the Interior The official newspaper Annual 2015 Visitor Guide Park Information and Maps The Best of Both Worlds What Lies Below? From Tipis to Tours Back From the Brink Wind Cave National Park is host to Wind Cave is considered sacred and Many national parks are great places one of the longest and most complex culturally significant to many American to view wildlife. However, that has caves in the world. Currently over 143 Indians, and throughout the centuries, not always been the case. In the early miles of twisting passageways reside many tribes lived and traveled within 1900s, many animal populations neared under only 1.2 square miles of surface what would become Wind Cave extinction because of loss of habitat or area, creating a maze of tunnels deep National Park. Who first discovered hunting pressures. below the park's rolling hills. The cave Wind Cave is lost to time, but in 1881, is famous for a rare formation known Tom and Jesse Bingham rediscovered as boxwork. More boxwork is found in the cave when they were attracted Welcome to Wind Cave than all other caves in the to the entrance by whistling noises Wind Cave National Park! world combined. coming out of the cave. This national park is one of the oldest in Portions of Wind Cave are believed to In 1889, the South Dakota Mining the country. Established in 1903, it was the be over 300 million years old, making Company established a mining eighth national park created and the first set it one of the oldest known caves in the claim at Wind Cave and hired J.D. -
Caverns Measureless to Man: Interdisciplinary Planetary Science & Technology Analog Research Underwater Laser Scanner Survey (Quintana Roo, Mexico)
Caverns Measureless to Man: Interdisciplinary Planetary Science & Technology Analog Research Underwater Laser Scanner Survey (Quintana Roo, Mexico) by Stephen Alexander Daire A Thesis Presented to the Faculty of the USC Graduate School University of Southern California In Partial Fulfillment of the Requirements for the Degree Master of Science (Geographic Information Science and Technology) May 2019 Copyright © 2019 by Stephen Daire “History is just a 25,000-year dash from the trees to the starship; and while it’s going on its wild and woolly but it’s only like that, and then you’re in the starship.” – Terence McKenna. Table of Contents List of Figures ................................................................................................................................ iv List of Tables ................................................................................................................................. xi Acknowledgements ....................................................................................................................... xii List of Abbreviations ................................................................................................................... xiii Abstract ........................................................................................................................................ xvi Chapter 1 Planetary Sciences, Cave Survey, & Human Evolution................................................. 1 1.1. Topic & Area of Interest: Exploration & Survey ....................................................................12 -
Naica Mine M E X I
Cave of the Crystals grade 5 Revise / Sketch NEW ARIZONA MEXICO magine yourself one thousand feet underground, drilling a new tunnel in an old zinc and lead mine. I TEXAS Suddenly your drill bursts through the MEXICO rock wall. What you see takes your CHIHUAHUA breath away. Huge crystals fill a cave SONORA from end to end, floor to ceiling. They Chihuahua shimmer like moonlight. But before you can explore the cave, you are Naica Mine hit with air as hot as a blast from a furnace. Two mineworkers, Juan and Pedro Sanchez, discovered this amazing “Cave of the Crystals” in 2000 at the Naica Mine in the state of Chihuahua, The Cave of the Crystals is located in Mexico. They didn’t stay long, for the intenseSue heat Carlson 609 971 6828 the desert of northern drove them away. Mexico. The mine owners put an iron door at the mouth of the cave. Scientists came to study the cave, but because of the heat, they could stay inside for only a few minutes at a time. 28 5_RNLESE865836_U6SA27.indd 28 5/10/2012 6:28:25 AM Inside Mexico’s Cave of the Crystals Cave of the Crystals grade 5 Revise / Sketch Scientists found the crystals were made of selenite gypsum, a translucent, light-colored mineral. The cave had just the NEW right combination of minerals, water, and ARIZONA MEXICO temperature to grow the crystals. The cave had once been filled with water, and heat from the earth’s core kept the water at TEXAS MEXICO about 136 degrees Fahrenheit. -
November 21, 2008
Note venues and dates with care. The Explorers Club Tiburon, CA! Our next event is at 6:30 on Nov. 21, a Friday evening, Northern California Chapter at the Dana home. November 2008 NGS In color at our web site: http://www.diggles.com/ec/ Tiburon—November 21, 2008 Leela Hutchison The Cave of Crystals An Early Exploration of Gigantic ‘Gems’ In 1794, among trees and a spring, in the into a consultant to the owners of the mine low hills southwest of Chihuahua, Mexico, in the year 2000, when staying just across early prospectors found a vein of silver the Arizona border at Aqua Prieta—their ore exposed. They named the locale Naica mutual interest: visiting and helping the An enormous geode filled with huge selenite (a Tarahumara word for ‘shady place.’) It Tarahumaras of the Sierra Madre Occiden- crystals was discovered in 2000; our speaker was there in 2001. By 2008, suitably suited was one-hundred years later that a claim tal. He showed her some pictures of a new explorers continued observations. R F was made for a mine, and Naica became a chamber that had just been discovered, R F ISHER pueblo, a small town. Throughout the 20th more than twice as far below the surface! ISHER century and still, the mine has prospered Subsequently named the Cave of the Crys- as a world-leading lead, zinc, silver and tals, it is a phenomenal world-class won- gold resource. Extensive workings exist, derland of even larger crystals. interrupted only during the Mexican revo- Their meeting led to a discussion of how lution of the 1920s and ‘30s. -
Cave & Karst Resource Management Plan, Wind Cave National Park
Cave & Karst Resource Management Plan, Wind Cave National Park 2007 Cave and Karst Resource Management Plan, Wind Cave National Park CAVE AND KARST RESOURCE MANAGEMENT PLAN WIND CAVE NATIONAL PARK March 2007 Recommended By: ___________________________________________________________________ Physical Science Specialist, Date: Wind Cave National Park Concurred By: ___________________________________________________________________ Chief of Resource Management, Date: Wind Cave National Park Approved By: ___________________________________________________________________ Superintendent, Wind Cave National Park Date: 2 Cave & Karst Resource Management Plan, Wind Cave National Park 2007 Cave and Karst Resource Management Plan, Wind Cave National Park Table of Contents I. BACKGROUND....................................................................................................................................................... 4 A. PARK PURPOSE ................................................................................................................................................... 4 B. GEOGRAPHIC LOCATION & DESCRIPTION OF THE PARK ..................................................................................... 4 C. PARK SIGNIFICANCE ............................................................................................................................................ 4 D. SURFACE LAND MANAGEMENT RELATIONSHIP TO KARST............................................................................... 10 II. CAVE AND KARST RESOURCE -
Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico
minerals Review Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico Iván Jalil Antón Carreño-Márquez 1 , Isaí Castillo-Sandoval 2, Bernardo Enrique Pérez-Cázares 3, Luis Edmundo Fuentes-Cobas 2 , Hilda Esperanza Esparza-Ponce 2 , Esperanza Menéndez-Méndez 4, María Elena Fuentes-Montero 3 and María Elena Montero-Cabrera 2,* 1 Department of Engineering, Universidad La Salle Chihuahua, Chihuahua 31625, Mexico; [email protected] 2 Department of Environment and Energy, Centro de Investigación en Materiales Avanzados, Chihuahua 31136, Mexico; [email protected] (I.C.-S.); [email protected] (L.E.F.-C.); [email protected] (H.E.E.-P.) 3 Department of Computational Chemistry, Universidad Autónoma de Chihuahua, Chihuahua 31125, Mexico; [email protected] (B.E.P.-C.); [email protected] (M.E.F.-M.) 4 Department Physicochemical Assays, Instituto Eduardo Torroja de Ciencias de la Construcción, 28033 Madrid, Spain; [email protected] * Correspondence: [email protected] Abstract: Calcium sulfate (CaSO4) is one of the most common evaporites found in the earth’s crust. It can be found as four main variations: gypsum (CaSO4·2H2O), bassanite (CaSO4·0.5H2O), soluble Citation: Carreño-Márquez, I.J.A.; anhydrite, and insoluble anhydrite (CaSO4), being the key difference the hydration state of the Castillo-Sandoval, I.; Pérez-Cázares, sulfate mineral. Naica giant crystals’ growth starts from a supersaturated solution in a delicate B.E.; Fuentes-Cobas, L.E.; Esparza- thermodynamic balance close to equilibrium, where gypsum can form nanocrystals able to grow Ponce, H.E.; Menéndez-Méndez, E.; up to 11–12 m long. -
Caves and Karst
CAVES AND KARST An educational curriculum guide on cave and karst resources. 2 week unit Prepared by the National Park Service and their partners at the University of Colorado at Denver. NPS Photo by Rick Wood Page 1 of 120 Table of Contents 1. Foreword Page 3 2. National Standards Page 5 3. Caves and Karst Activity Objectives Page 10 4. Caves and Karst Activities and Lesson Plans Day 1: Interactive Reading Guide Page 14 Reading Guide - Teacher Version Reading Guide - Student Version Day 2: Making a Cave Page 35 Making a Cave - Teacher Version Making a Cave - Student Version Day 3 and 4: Growing Speleothems Page 46 Growing Speleothems - Teacher Version Growing Speleothems - Student Version Day 5: Speleothems: A Webquest Page 62 Speleothems Webquest - Teacher Version Speleothems Webquest - Student Version Day 6: Cave Life: A Jigsaw Activity Page 77 Cave Life - Teacher Version Cave Life - Activity Fact Cards Cave Life - Student Version Day 7, 8, and 9: Present a Cave Page 92 Present a Cave - Teacher Version Present a Cave - Activity Fact Cards: 8 NPS Caves Present a Cave - Student Worksheet Present a Cave - Peer Evaluation Form Present a Cave - Group Member Evaluation Form Day 10: Cave Quiz Game Page 110 (Access game via Views DVD or website) Cave Quiz Game - Teacher Version Page 116 NPS Photo by Rick Wood 5. Glossary of Terms Foreword “Views of the National Parks” (Views) is a multimedia education program that presents stories of the natural, historical, and cultural wonders associated with America’s parks. Through the use of images, videos, sounds and text, Views allows the public to explore the national parks for formal and informal educational purposes. -
Karst Features in the Black Hills, Wyoming and South Dakota- Prepared for the Karst Interest Group Workshop, September 2005
193 INTRODUCTION TO THREE FIELD TRIP GUIDES: Karst Features in the Black Hills, Wyoming and South Dakota- Prepared for the Karst Interest Group Workshop, September 2005 By Jack B. Epstein1 and Larry D. Putnam2 1U.S. Geological Survey, National Center, MS 926A, Reston, VA 20192 2Hydrologist, U.S. Geological Survey, 1608 Mountain View Road, Rapid City, SD 57702. This years Karst Interest Group (KIG) field trips will demonstrate the varieties of karst to be seen in the semi-arid Black Hills of South Dakota and Wyoming, and will offer comparisons to karst seen in the two previous KIG trips in Florida (Tihansky and Knochenmus, 2001) and Virginia (Orndorff and Harlow, 2002) in the more humid eastern United States. The Black Hills comprise an irregularly shaped uplift, elongated in a northwest direction, and about 130 miles long and 60 miles wide (figure 1). Erosion, following tectonic uplift in the late Cretaceous, has exposed a core of Precambrian metamorphic and igneous rocks which are in turn rimmed by a series of sed- iments of Paleozoic and Mesozoic age which generally dip away from the center of the uplift. The homocli- nal dips are locally interrupted by monoclines, structural terraces, low-amplitude folds, faults, and igneous intrusions. These rocks are overlapped by Tertiary and Quaternary sediments and have been intruded by scattered Tertiary igneous rocks. The depositional environments of the Paleozoic and Mesozoic sedimen- tary rocks ranged from shallow marine to near shore-terrestrial. Study of the various sandstones, shales, siltstones, dolomites and limestones indicate that these rocks were deposited in shallow marine environ- ments, tidal flats, sand dunes, carbonate platforms, and by rivers. -
The Caves & Karst Edition
A Tale of Two Caves: How Is Hurricane Crawl Cave Different From Crystal Cave? Photo courtesy of Dave Bunnell, Under Earth Images. Meet the Scientists Joel D. Despain, Hydrologist: My favorite scientific experiences involve understanding the geomorphic history of a given cave or cave area. Some geomorphic questions are, “Why did the cave form, and why did it form with these particular shapes and patterns? Is it random?” It turns out that caves form in specific ways that tell us about past conditions. The history of the cave, the structure of the rock, the hydrology of the region, the gradient, and other factors all play big roles. Cave geologists are determining different types of caves and how they develop with greater precision every year. They do this through a better understanding of the shapes, forms, and patterns found within caves. This research is creating a much better understanding of caves that then informs our understanding and knowledge of regional geology and geologic history. Benjamin W. Tobin, Hydrologist: Each science experience is amazing, interesting, and fun in its own way. If I had to choose, however, my favorite would be conducting dye traces at the Grand Canyon. This work involves dumping a colored non-harmful dye into the ground up on the plateau above the canyon, then monitoring springs in the canyon to determine where the dye showed up. This is simple science. But the results tell us an incredible amount about how water moves below our feet and it never seems to do what we expect. Greg M. Stock, Geologist: My favorite science experience was mapping caves in Sequoia with Mr. -
2019-3 PGS Newsletter
MARCH 2019 PGS NEWSLETTER VOL LXXI NO 7 Could Earth’s Long-Wavelength March 20, 2019 (Degree-2) Mantle Structure Be Social hour 6:00 PM Stable Through Time? Dinner 7:00 PM Program 8:00 PM Dinner costs $30.00 per person $10.00 student member Reservations Email your name and number of attendees to: pgsreservations @gmail.com You can also reserve and pay via PayPal at: https://www.pittsburgh Dr. Mathew Domeier geologicalsociety.org/ Researcher, Centre for Earth NEW LOCATION Cefalo's Banquet & Evolution and Dynamics (CEED), Event Center, University of Oslo, Norway Carnegie PA Deadline for Reservations: Wednesday, March 13. , Speaker Abstract At the base of Earth’s mantle, just above the boundary with the core, lie two large and nearly antipodal provinces characterized by anomalously slow seismic wave speeds, termed the Large Low Shear-wave Velocity Provinces (LLSVPs). One of these structures lies beneath Africa, and the other beneath the Pacific Ocean. Accumulating evidence has increasingly revealed that the LLSVPs play an important role in mantle dynamics, most notably in that they are spatially associated with most deep- seated mantle plumes, and they coincide with the broad, antipodal upwellings in Earth’s degree-2 mantle flow. In affecting large-scale convection in the mantle, and the nucleation of plumes that can fragment the lithosphere, these lowermost mantle structures may furthermore influence long-term plate motions. A key question is therefore: how stable have these features been through time? Here I discuss multiple independent lines of evidence that indicate that the LLSVPs have been in approximately the same position for the last 300 Ma, and possibly considerably longer. -
Mcgill University Alumni Newsletter #23 January 2020
McGill University Alumni Newsletter #23 January 2020 In 2008 and 2009, renewed exploration by Osisko Mining revealed an untapped new gold deposit, estimated at approximately 9 million ounces, beneath the town of Malartic. QC. The company would become Canada's largest ever open pit gold mine. The mine was developed within just six years after the first exploration drillholes in 2005. The first gold pour was in April 2011, and commercial production began in May 2011. Chemical Formula: Au Locality: Many places in the world. Name Origin: Anglo Saxon, of uncertain origin. Gold is a chemical element with symbol Au (from Latin: aurum) and atomic number 79. It is a bright yellow dense, soft, malleable and ductile metal. The properties remain when exposed to air or water. Chemically, gold is a transition metal and a group 11 element. It is one of the least reactive chemical elements, and is solid under standard conditions. The metal therefore occurs often in free elemental (native) form, as nuggets or grains, in rocks, in veins and in alluvial deposits. It occurs in a solid solution series with the native element silver (as electrum) and also naturally alloyed with copper and palladium. Less commonly, it occurs in minerals as gold compounds, often with tellurium (gold tellurides). Gold’s atomic number of 79 makes it one of the higher atomic number elements that occur naturally in the universe, and is traditionally thought to have been produced in supernova nucleosynthesis to seed the dust from which the Solar System formed. Because the Earth was molten when it was just formed, almost all of the gold present in the Earth sank into the planetary core.