A Geochemical Study of Speleothems and Cave Waters in Basaltic Caves at Lava Beds National Monument, Northern California, USA

Total Page:16

File Type:pdf, Size:1020Kb

A Geochemical Study of Speleothems and Cave Waters in Basaltic Caves at Lava Beds National Monument, Northern California, USA A geochemical study of speleothems and cave waters in basaltic caves at Lava Beds National Monument, Northern California, USA by Joshua A. Ford B.A., Hanover College, 2018 A THESIS submitted in partial fulfillment of the requirements for the degree MASTER OF SCIENCE Department of Geology College of Arts and Sciences KANSAS STATE UNIVERSITY Manhattan, Kansas 2020 Approved by: Approved by: Co-Major Professor Co-Major Professor Matthew Brueseke Saugata Datta Copyright © Joshua Ford 2020. Abstract Lava caves within Lava Beds National Monument (LBNM), CA, were selected as terrestrial analog sites for caves observed on other planetary bodies. The lava caves at LBNM were found to contain active microbial communities, including colorful biofilms. Additionally, the caves were discovered to host a variety of morphologically distinct secondary mineral deposits known as speleothems. Speleothems and co-located cave waters were collected to determine their compositions and assess geochemical biosignatures. Speleothems were analyzed for mineralogical, elemental, and internal stratigraphic contents. Cave waters were analyzed for major elements, major ions, DOC, and stable isotopes. Speleothems were found to be comprised primarily of opal-A and calcite, with elemental chemistries dominated by SiO2 and CaO, alongside lesser concentrations of MgO. Speleothem formation was ultimately interpreted to be driven by both inorganic and biological factors, including availability of water, extent of evaporation, and nucleation influenced by microbial bioaccumulation. Mineral precipitation likely occurs due to evaporation of water films supplied by condensation and capillary action, with opal favored in wet conditions and calcite in dry conditions, where increased evaporative concentration favors the precipitation of calcite and Mg carbonate. Microbes likely mediate precipitation through nucleation of porous opal by bound silanol in microbial extracellular products. This creates a microsystem wherein autotrophic bacteria may encourage carbonate mineral precipitation via CO2 consumption increasing pH, and may be reflected in the presence of both microstromatolite-like opal and calcite lamina and a predominance of DOC in cave waters. These findings contribute to the further understanding and characterization of lava cave speleothems as potential biosignature targets. Table of Contents List of Figures ..................................................................................................................................x List of Tables ............................................................................................................................... xiii Acknowledgements ...................................................................................................................... xiv CHAPTER 1 – Introduction and Background ............................................................................1 1.1 Introduction to Lava Caves, Extraterrestrial Lava Caves, and BRAILLE ..........................1 1.2 Lava Cave Secondary Mineral Deposits – Speleothems .....................................................6 1.3 Mineralogical Variations among Speleothems ....................................................................6 1.4 Occurrence and Role of Water in Lava Caves .....................................................................8 1.5 Speleothem Formation Processes ........................................................................................9 1.6 Microbial Processes Influencing Speleothem Formation ..................................................10 1.7 Hypotheses and Objectives ................................................................................................13 CHAPTER 2 – Study Area..........................................................................................................16 2.1 Recent Medicine Lake Volcanism .....................................................................................17 2.2 Ground Water Hydrology of Tule Lake Subbasin and LBNM ..........................................18 2.3 Lava Cave Organisms ........................................................................................................19 2.3.1 Prokaryotes and Archaea .......................................................................................19 2.3.2 Eukaryotes..............................................................................................................20 2.3.3 Plants ......................................................................................................................21 CHAPTER 3 – Methods ..............................................................................................................22 3.1 Sample Collection ..............................................................................................................22 iv 3.2 Sample Preparation and X-Ray Diffraction Analysis ........................................................27 3.3 Clay Fraction ......................................................................................................................27 3.4 X-Ray Fluorescence ...........................................................................................................28 3.5 Thin Sections and Petrography ..........................................................................................29 3.6 Electron Microprobe ..........................................................................................................29 3.7 Water Chemistry ................................................................................................................30 3.7.1 Ion Chromatography ..............................................................................................30 3.7.2 Alkalinity ...............................................................................................................30 3.7.3 ICP-MS ..................................................................................................................30 3.7.4 TOC, DOC, and TDN ............................................................................................30 3.7.5 δ18O and δ2H Stable Isotopes .................................................................................31 3.8 Geochemical Modeling ......................................................................................................31 3.9 Scanning Electron Microscopy ..........................................................................................31 CHAPTER 4 – Results.................................................................................................................32 4.1 Variations in Speleothem Morphology ..............................................................................32 4.1.1 Cave Basalt ............................................................................................................32 4.1.2 Crusts .....................................................................................................................33 4.1.3 Polyps .....................................................................................................................34 4.1.4 Cauliflower ............................................................................................................34 4.1.5 Coralloids ...............................................................................................................35 4.1.6 Gours ......................................................................................................................36 v 4.2 Speleothem and Basalt Mineralogy ...................................................................................37 4.2.1 Cave Basalt ............................................................................................................37 4.2.2 Speleothems ...........................................................................................................38 4.2.3 Museum-Grade Opal Standards .............................................................................39 4.2.4 Crusts .....................................................................................................................40 4.2.5 Polyps .....................................................................................................................41 4.2.6 Cauliflower ............................................................................................................41 4.2.7 Coralloids ...............................................................................................................42 4.2.8 Gours ......................................................................................................................43 4.3 Clay Mineralogy ................................................................................................................44 4.4 Petrographic Analysis of LBNM Speleothems and Cave Basalt .......................................44 4.4.1 Cave Basalt ............................................................................................................44 4.4.2 Crusts, Cauliflower, Polyps, Coralloids, and Gours ..............................................45 4.4.3 Volcanic Fragment Inclusions within Speleothems ...............................................51 4.5 Cave Bare Basalt and Speleothem Elemental Composition ..............................................52 4.5.1 Cave Basalt ............................................................................................................52 4.5.2 Crusts .....................................................................................................................55
Recommended publications
  • Casleguard Cave 2005
    Castleguard Cave 2005 First ascent of the 200-foot aven Text by Marek Vokáˇc Photos by Christian Rushfeldt, Bjørn Myrvold, Jørn Halvorsen, Marek Vokáˇc First edition October 27, 2006 Copyright notice: Overall copyright © 2006 Marek Vokáˇc. Photographers retain their copy- right © to individual images as specified in photo credits/captions. Permission is generally granted for individual, non-commercial use of this report, provided due credit is given. Parks Canada is additionally granted permission for other non-commercial use and distribution. Author contact: Marek Vokáˇc Thorleifs Allé 5c 0489 Oslo Norway email: [email protected] Telephone: +47 934 92 857 Cover photo: Marek Vokáˇcclimbing the aven, by Christian Rushfeldt (CC05-064) Dedicated to all whose generous support made this trip possible, and a success: my wife and children; the team; their families; and our colleagues and employers Introduction Castleguard Cave lies in the heart of the Rocky Mountains, close to the Saskatchewan Glacier. To get to the cave from Calgary, one drives the beautiful Icefields Parkway, past Lake Louise and Banff, preferably staying at the Saksatchewan Crossing hotel. Getting to the cave entrance is a full-day ski trip. The cave itself was known early in the 1900’s, and was visited by tourists with horses and mules. The biggest attraction were the sudden floods coming out of the entrance, where the dry opening would change into a roaring river in a few seconds. Modern cave exploration started in 1967, during the summer. The explorers were caught by a sudden rise in the water and trapped inside the first drop. After 18 hours the water level dropped enough for them to get out; soon after that, the waters rose again and ran for weeks.
    [Show full text]
  • Museum of Natural History & Science Interpretation Guide for the Cavern
    Museum of Natural History & Science Interpretation Guide for The Cavern A cave is a naturally occurring hole in the ground large enough to be explored by humans. Caves can be found on every continent in the world. Caves, along with the objects found within them, are extremely fragile and take millions of years to form. They are home to unique organisms—many of which are still unknown to science; they are archaeological sites that preserve our cultural heritage; and geologic laboratories that demonstrate how water can both dissolve and deposit rock. Caves are a vital and non-renewable resource that must be conserved and protected. The Cavern is a recreation of a Kentucky limestone dissolution cave. It is the largest artificial cave in the United States—and some say the world—containing 535 feet of passage in an area 44 feet wide, 24 feet high and 64 feet long. Parts of the cave were modeled after two caves in Kentucky: Teamers Cave in Rockcastle County and Dyches Bridge Cave in Pulaski County. By modeling our cavern after these two caves, our dissolution cave has a realistic appearance. A dissolution cave is by far the most common type of cave. They can be found throughout the world if the right conditions present themselves. The formation of a dissolution cave requires four basic elements: rock, water, carbon dioxide and time. • Rock, especially carbonate rocks, such as limestone, is the first ingredient. These types of rocks were formed hundreds of millions of years ago. It is in the seas surrounding the continents that limestone is formed.
    [Show full text]
  • Growth Mechanisms of Speleothems in Castleguard Cave, Columbia Icefields, Alberta, Canada
    Arctic and Alpine Research ISSN: 0004-0851 (Print) 2325-5153 (Online) Journal homepage: https://www.tandfonline.com/loi/uaar19 Growth Mechanisms of Speleothems in Castleguard Cave, Columbia Icefields, Alberta, Canada T. C. Atkinson To cite this article: T. C. Atkinson (1983) Growth Mechanisms of Speleothems in Castleguard Cave, Columbia Icefields, Alberta, Canada, Arctic and Alpine Research, 15:4, 523-536 To link to this article: https://doi.org/10.1080/00040851.1983.12004379 Copyright 1983 Regents of the University of Colorado Published online: 01 Jun 2018. Submit your article to this journal Article views: 64 View related articles Citing articles: 4 View citing articles Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=uaar20 Arctic and Alpine Research, Vol. 15, No.4, 1983, pp. 523-536 GROWTH MECHANISMS OF SPELEOTHEMS IN CASTLEGUARD CAVE, COLUMBIA ICEFIELDS, ALBERTA, CANADA* T. C. ATKINSON School ofEnvironmental Sciences, University ofEast Anglia, Norwich NR4 7TJ, England, U.K. ABSTRACT In spite of its location beneath high alpine terrain and active glaciers, Castleguard Cave contains many actively growing calcite'speleothems. Four hypotheses as to their growth mechanism were tested against field data on water chemistry, temperatures, CO 2 content of cave air, and evaporation rates. The hypotheses were (1) that a biogenic source of high PC02 is unlikely, so calcite deposition by CO 2 degassing would require a nonbiogenic source; (2) warming of water after entering the cave, or in passage through the rocks above it might cause calcite supersaturation; (3) calcite might be deposited because of evaporation of seep­ age; and (4) waters dissolving several Ca-bearing minerals might precipitate calcite as the least soluble by the common-ion effect.
    [Show full text]
  • Caves of Missouri
    CAVES OF MISSOURI J HARLEN BRETZ Vol. XXXIX, Second Series E P LU M R I U BU N S U 1956 STATE OF MISSOURI Department of Business and Administration Division of GEOLOGICAL SURVEY AND WATER RESOURCES T. R. B, State Geologist Rolla, Missouri vii CONTENT Page Abstract 1 Introduction 1 Acknowledgments 5 Origin of Missouri's caves 6 Cave patterns 13 Solutional features 14 Phreatic solutional features 15 Vadose solutional features 17 Topographic relations of caves 23 Cave "formations" 28 Deposits made in air 30 Deposits made at air-water contact 34 Deposits made under water 36 Rate of growth of cave formations 37 Missouri caves with provision for visitors 39 Alley Spring and Cave 40 Big Spring and Cave 41 Bluff Dwellers' Cave 44 Bridal Cave 49 Cameron Cave 55 Cathedral Cave 62 Cave Spring Onyx Caverns 72 Cherokee Cave 74 Crystal Cave 81 Crystal Caverns 89 Doling City Park Cave 94 Fairy Cave 96 Fantastic Caverns 104 Fisher Cave 111 Hahatonka, caves in the vicinity of 123 River Cave 124 Counterfeiters' Cave 128 Robbers' Cave 128 Island Cave 130 Honey Branch Cave 133 Inca Cave 135 Jacob's Cave 139 Keener Cave 147 Mark Twain Cave 151 Marvel Cave 157 Meramec Caverns 166 Mount Shira Cave 185 Mushroom Cave 189 Old Spanish Cave 191 Onondaga Cave 197 Ozark Caverns 212 Ozark Wonder Cave 217 Pike's Peak Cave 222 Roaring River Spring and Cave 229 Round Spring Cavern 232 Sequiota Spring and Cave 248 viii Table of Contents Smittle Cave 250 Stark Caverns 256 Truitt's Cave 261 Wonder Cave 270 Undeveloped and wild caves of Missouri 275 Barry County 275 Ash Cave
    [Show full text]
  • 871 Definitions
    433.871 Definitions. As used in this chapter, the following words shall have the meanings stated unless the context requires otherwise: (1) "Cave" means any naturally occurring void, cavity, recess, or system of interconnecting passages beneath the surface of the earth containing a black zone including natural subterranean water and drainage systems, but not including any mine, tunnel, aqueduct, or other man-made excavation, which is large enough to permit a person to enter. The term "cave" includes or is synonymous with "cavern." (2) "Commercial cave" means any cave utilized by the owner for the purposes of exhibition to the general public, whether as a profit or nonprofit enterprise, wherein a fee for entry is collected. (3) "Gate" means any structure or device situated so as to limit or prohibit access or entry to any cave. (4) "Person" or "persons" means any individual, partnership, firm, association, trust, or corporation or other legal entity. (5) "Owner" means a person who owns title to land wherein a cave is located, including a person who owns title to a leasehold estate in the land and specifically including the Commonwealth and any of its agencies, departments, boards, bureaus, commissions, or authorities as well as counties, municipalities and other political subdivisions of the Commonwealth. (6) "Speleothem" means a natural mineral formation or deposit occurring in a cave. This shall include or be synonymous with, but not restricted to stalagmite, stalactite, helectite, shield, anthodite, gypsum flower and needle, angel's hair, soda straw, drapery, bacon, cave pearl, popcorn, coral, rimstone dam, column, palette, flowstone, et cetera.
    [Show full text]
  • World Heritage Caves and Karst: a Thematic Study
    World Heritage Convention IUCN World Heritage Studies 2008 Number Two World Heritage Caves and Karst A Thematic Study IUCN Programme on Protected Areas A global review of karst World Heritage properties: present situation, future prospects and management requirements . IUCN, International Union for Conservation of Nature Founded in 1948, IUCN brings together States, government agencies and a diverse range of non-governmental organizations in a unique worldwide partnership: over 1000 members in all, spread across some 140 countries. As a Union, IUCN seeks to influence, encourage and assist societies throughout the world to conserve the integrity and diversity of nature and to ensure that any use of natural resources is equitable and ecologically sustainable. A central Secretariat coordinates the IUCN Programme and serves the Union membership, representing their views on the world stage and providing them with the strategies, services, scientific knowledge and technical support they need to achieve their goals. Through its six Commissions, IUCN draws together over 10,000 expert volunteers in project teams and action groups, focusing in particular on species and biodiversity conservation and the management of habitats and natural resources. The Union has helped many countries to prepare National Conservation Strategies, and demonstrates the application of its knowledge through the field projects it supervises. Operations are increasingly decentralized and are carried forward by an expanding network of regional and country offices, located principally in developing countries. IUCN builds on the strengths of its members, networks and partners to enhance their capacity and to support global alliances to safeguard natural resources at local, regional and global levels.
    [Show full text]
  • Geology of Caves Geology of Caves by W
    U.S. Department of the Interior / U.S. Geological Survey Geology of Caves Geology of Caves by W. E. Davies and I. M. Morgan A cave is a natural opening in the ground extending beyond the zone of light and large enough to permit the entry of man. Occurring in a wide variety of rock types and caused by widely differing geological proc­ esses, caves range in size from single small rooms to intercorinecting passages many miles long. The scientific study of caves is called speleology (from the Greek words spelaion for cave and logos for study). It is a composite science based on geology, hydrology, biology, and archaeology, and thus holds special interest for earth scientists of the U.S. Geological Survey. Caves have been natural attractions since prehistoric times. Prolific evidence of early man's interest has been discovered in caves scattered throughout the world. Fragments of skeletons of some of the earliest manlike creatures (Australopithecines) have been discovered in cave deposits in South Africa, and the first evidence of primitive Neander­ thal Man was found in a cave in the Meander Valley of Germany. Cro-Magnon Man created his remarkable murals on the walls of caves in southern France and northern Spain where he took refuge more than 10,000 years ago during the chill of the ice age. Interest in caves has not dwindled. Although firm figures for cave visitors are not available, in 1974 about 1.5 million people toured Mammoth Cave in Kentucky, and more than 670,000 visited Carlsbad Caverns in New Mexico, two of the most famous caves in the United States.
    [Show full text]
  • Cavern Geology Lesson Plan 1
    Thank you to the Sierra Nevada Recreation Corporation: Moaning Cavern, Black Chasm Cavern and California Cavern for permission to use their classroom lesson plan material. Cavern Geology Lesson 1: What is a Cavern? OBJECTIVE Students will learn to identify the different types of caves. BACKGROUND INFORMATION Cave or Cavern? Is there a difference between a cave and a cavern? This is a frequently asked question, and many people use the terms interchangeably. However, there is a difference. A cave is any cavity in the ground that is large enough that some portion of it will not receive direct sunlight. There are many types of caves (discussed in this lesson plan). A cavern is a specific type of cave, naturally formed in soluble rock with the ability to grow speleothems. So, although a cavern can accurately be called a cave (since it is a type of cave), all caves cannot be called caverns. Caves Caves can be classified into two main categories known as primary and secondary. This classification is based on their origin. Primary caves are developed as the host rock is solidifying. Examples of primary caves include lava tubes and coral caves (descriptions follow). Secondary caves are carved out of the host rock after it has been deposited or consolidated. Most caves fall in the secondary category. However, some primary caves may later be enlarged by the forces associated with secondary cave development. Listed here are the main types of caves, and how they are formed: Coral Caves When colonies of coral in shallow water expand and unite, they form lacy or bulbous walls around an open area.
    [Show full text]
  • NARACOORTE CAVES NATIONAL PARK: VISITOR FACILITY UPGRADES Deborah Carden
    Journal of the Australasian Cave and Karst Management Association No. 105 December 2016 Australia Post- Print Post Approved: PP381624/02050. ISSN 1835-5374 Published Quarterly The ACKMA Journal ACKMA Inc. OFFICE BEARERS 2016-17 Official Publication of the Australasian Cave and President Karst Management Association Incorporated Dale Calnin Email: [email protected] Published quarterly in March, June, September and New Zealand Vice President December Neil Collinson Email: [email protected] The opinions expressed in the ACKMA Journal are those of the individual authors and not necessarily Australian Vice President those of ACKMA Inc. or its officers. John Brush Email: [email protected] EDITOR: Steve Bourne Executive Officer SUB EDITORS: Tony Culberg, Andy Spate Dan Cove Email: [email protected] Photos taken by the authors or editor unless Treasurer and Membership Officer otherwise acknowledged. Deborah Carden Email: [email protected] PRINTER: Hansen Print, Smith Street, Naracoorte, South Australia 5271. Ph: (08) Publications Officer and ASF Liaison Officer 87623699 Steve Bourne Email: [email protected] ACKMA Inc. is cross affiliated or otherwise Committee member associated with: Scott Melton Email: [email protected] Australian Speleological Federation, New Zealand Speleological Society, Australasian Bat Society, Committee Member The WCPA Working Group on Cave and Karst Tim Moulds Email: [email protected] Protection, Guiding Organisations Australia, Bat Conservation International, American Cave Committee Member Conservation Association, International Show Ann Augusteyn Email: [email protected] Caves Association, Cave Diving Association of Australia, The Malaysian Karst Society, The Webmaster Jenolan Caves Historical & Preservation Society Rauleigh Webb Email: [email protected] and the USA National Speleological Society Cave Conservation and Management Section Public Officer LIFE MEMBERS of ACKMA Inc.
    [Show full text]
  • Spelunker Speak 2 Cave Vocabulary
    Spelunker Speak 2 Cave Vocabulary Materials: Vocabulary List = Crossword Puzzle = Pens and/or Pencils Students should solve the crossword puzzle using words from the Cave Vocabulary list. These words can also be used for the bulletin board in Activity 1. Answers: Across Down 2. Calcite 1. Flowstone 4. Cave Coral 2. Column 6. Karst 3. Drapery 7. Speleothem 5. Aragonite 10. Shields 8. Helictites 11. Stalagmite 9. Soda Straws 12. Rimstone Dams 13. Spelunker 14. Stalactite 2-1 Indiana Bats, Kids & Caves - Oh My! 2-2 Indiana Bats, Kids & Caves - Oh My! Name ________________________________ Spelunker Speak 2 Words every spelunker should know... Aragonite A cave mineral, which often forms needle-like crystals. Calcite A common crystalline form of calcium carbonate. Cave coral Also known as “popcorn”; small knobby clusters formed by seep- ing water. Column When a stalactite and a stalagmite grow together from the floor to the ceiling. Drapery A speleothem formed when water deposits calcite in thin sheets that hang in delicate folds. Flowstone Resembling frozen waterfalls, form when water flows down walls, over floors and older formations, building up sheets of calcite like icing on a cake. Helicitites Small twisted structures projecting from ceilings, walls and the floor of caves that seem to defy the laws of gravity. Formed by seeping water, they project at all angles. Karst An irregular limestone region with sinks, underground streams, and caverns. Rimstone dams Step-like terraces along streams and on cave floors that enclose pools of water. Shields Flat semi-circular calcite sheets formed by water seeping from a thin crack.
    [Show full text]
  • Small Scale Terraces and Isolated Rimstone Pools On
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by ZRC SAZU Publishing (Znanstvenoraziskovalni center -COBISS: Slovenske 1.01 akademije znanosti in... SMALLSCALE TERRACES AND ISOLATED RIMSTONE POOLS ON STALAGMITES IN CAVES EXHIBIT STRIKING SIMILARITY TO LARGESCALE TERRACE LANDSCAPES AT HOT SPRINGS DROBNE SIGASTE TERASE NA STALAGMITIH SO PRESENETLJIVO PODOBNE VELIKIM TERASAM, KI RASTEJO OB TERMALNIH KRAŠKIH IZVIRIH Wolfgang DREYBRODT 1,2 & Franci GABROVŠEK 2 Abstract UDC 911.2:551.435.843 Izvleček: UDK 911.2:551.435.843 Wolfgang Dreybrodt & Franci Gabrovšek: Small-scale ter- Wolfgang Dreybrodt & Franci Gabrovšek: Drobne sigaste ter- races and isolated rimstone pools on stalagmites in caves ex- ase na stalagmitih so presenetljivo podobne velikim terasam, hibit striking similarity to large-scale terrace landscapes at ki rastejo ob termalnih kraških izvirih hot springs V prispevku poročamo o sigastih terasah reda velikosti centi- We report on sinter terrace forms on the centimetre scale ob- metra, ki smo jih opazili na stalagmitu v Škocjanskih jamah. served on the top and at the base of a stalagmite in Škocjanske Pregrade drobnih sigovih ponvic tvorijo mrežo teras, ki močno jame (Škocjan caves). #ese exhibit connected rimstone dams, spominja na terase v velikem merilu, kot jih najdemo na mes- forming a net-like pattern with active water pools inside. #e tih, kjer se kalcit izloča iz visoko prenasičenih vod termalnih form is similar to those seen at the large travertine terraces, izvirov. Precej drugačne, izolirane sigove ponvice velikosti ne- which form by precipitation of calcite from spring waters high- kaj centimetrov, pa smo našli na stalagmitih v jami Dimnice.
    [Show full text]
  • Modelling of Calcium Carbonate Precipitation in Natural
    MODELLING OF CALCIUM CARBONATE PRECIPITATION IN NATURAL KARST ENVIRONMENTS UNDER HYDRODYNAMIC AND CHEMICAL KINETIC CONTROL A Thesis Presented to The Graduate Faculty of The University of Akron In Partial Ful¯llment of the Requirements for the Degree Master of Science Brad L Justice May, 2006 MODELLING OF CALCIUM CARBONATE PRECIPITATION IN NATURAL KARST ENVIRONMENTS UNDER HYDRODYNAMIC AND CHEMICAL KINETIC CONTROL Brad L Justice Thesis Approved: Accepted: Advisor Dean of the College Dr. Curtis Clemons Dr. Ronald F. Levant Co-Advisor Dean of the Graduate School Dr. Eric Wright Dr. George R. Newkome Faculty Reader Date Dr. Gerald Young Department Chair Dr. Kevin Kreider ii ABSTRACT Rimstone dams are barriers composed mainly of calcium carbonate deposited from solution in ground and surface waters. These structures form a subclass of travertine formations which include owstone and stalactites, and often appear in close proxim- ity to these features. The initial formation of rimstone dams requires some degree of cave slope, a semi-continuous ow of water, and the preexistence of irregularities in the cave oor. These dams develop at heights from a few millimeters to several me- ters within free-surface streams, and create a self-propagating dam and pool structure which grows upward. The genesis and evolution of rimstone dams is theorized to be the result of hydrodynamic and chemical-kinetic control. The purpose of this paper is to develop a model, the scope of which encompasses both hydrodynamics and the reactive transport, which is qualitatively consistent with observed and experimentally derived results, and method for analyzing the mechanism governing the formation of these unique rimstone features.
    [Show full text]