Iola Quadrangle, Kansas

Total Page:16

File Type:pdf, Size:1020Kb

Iola Quadrangle, Kansas DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR ECONOMIC GEOLOGY IOLA QUADRANGLE, KANSAS BY GEORGE I. ADAMS, ERASMUS HAWORTH, AND W. R. CRANE WASHINGTON GOVERNMENT PRINTING OFFICE 1904 *.., ERRATA. [Bull. U. S. Gteol. Survey No. 238.] The work of Mr. F. C. Schrader in the adjacent Independence and Parsons quadrangles during- the season of 1904 shows that certain mis- correlations were made in the survey of the lola quadrangle. The necessary corrections have been made on the maps (Pis. I and II), and the data for correcting- the text and Pis. Ill and IV are given below: PL III,-for Drum read Dennis. for Cherryvale read Galesburg. for Dennis read Mound Valley. for Galesburg read Laclore. PL IV, for Drum read Dennis. for Dennis read Mound Valley. Page 3, line 20, for Galesburg read Ladore. line 21, for Dennis read Mound Valley, line 22, for Cherryvale read Galesburg. line 23, for Drum read Dennis. Page 18, paragraph 1, line 10, for Galesburg read Ladore. line 11, for Dennis read Mound Valley. for Cherryvale read Galesburg. for Drum read Dennis. paragraph 4, line 1, for Galesburg read Ladore. paragraph 5, line 1, for Dennis read Mound Valley, paragraph 6, line 1, for Cherryvale read Galesburg. Page 19, paragraph 1, line 1,/or Drum read Dennis, line 7, for Drum read Dennis, paragraph 2, line 3, for Drum read Dennis. line 4, for Dennis read Mound Valley, line 5, for Galesburg read Ladore. for Cherryvale read Galesburg. paragraph 3, line 2, for Drum read Dennis. Page 21,-paragraph 5, line 5, 'for Galesburg read Ladore. .for Dennis read Mound Valley. for Cherryvale read Galesburg. for Drum read Dennis. Page 22, line 17, for Drum read Dennis. line 18, for Cherryvale read Galesburg. line 19, for Dennis read Mound Valley, line 20, for Galesburg read Laclore. Page 75, paragraph 2, line 3, for Shaw read Dennis. Page 79, line 14 from bottom, for Dennis read Mound Valley. for Drum read Dennis. CONTENTS. PllgO. Letter of transmittal...................................................... 9 Introduction, by George I. Adams ........................................ 11 Location of area described .......--........ ...............-----...---. 11 £» General statement".............. .* .................................... 12 Geology of the lola quadrangle, by George I. Adams ....................... 14 Surface features ...................................................... 14 Description of formations..................:...............-.......... .15 Mississippian series.........\..................................... 15 Boone formation ............................................. .15 Pennsylvania!! series ......................-.-..------..---....-.. 16 Cherokee shale .............................................. 16 Fort Scott limestone.......................................... 16 Labette shale ................................................ 17 Pawnee limestone............................................ 17 Bandera shale ............................................... 17 Parsons limestone............................................. !17 Dudley shale................................................. 17 Bronson formation ........................................... .17 Hertha limestone ............................................ 18 .: Galesburg shale.............................................. 18 Dennis limestone............................................. 18 Cherry vale shale.............................................. 18 Drum limestone...........................,-................... .1.9 Chanute shale ............................................... 19 lola limestone ............................................... 19 Concrete shale ....................:......:................... 20 .Alien limestone .............................................. 20 fc Vilas shale .................................................. 20 * ' Piqua limestone.............................................. 20 Alluvium........................................................ 21 Correlation and correction of faunal lists............................... 2.1 General structure..................................................... 23 Origin of oil and gas.............................................. 24 Relations of the oil- and gas-bearing sandstones .................... 25 Mineral resources and their utilization, by Erasmus Havvorth and George I. Adams, with sections by W. B. Crane ............................... 30 Oil and gas .......................................................... 30 Historical........................................................ 30 lola and Laharpe.............................................. 30 Humboldt................................................... 31 Chanute..................................................... 32 Erie......................................................... 34 [ Moran....................................................... 34 f Bronson, Elsrnore, Savonburg, and Stark ...................... 34 3 4 CONTENTS. Mineral resources and their utilization, etc. Continued. Page. Oil and gas Continued. Production ...................................................... 34 Oil.......................................................... 34 Gas ....;.................................................. 37 Gas-producing territory....................................... 38 Utilization of gas in zinc smelting ................................. 40 Development of the industry.................................. 40 Method of smelting .......................................... 42 Production of spelter in 1902 .................................. 43 Phenomena of gas wells, by George I. Adams ...................... 43 Static or closed pressure ...................................... 45 Dynamic or open-flow pressure.................'................ 47 Pressure and flow in pipes ............... ..................... 50 * Minute pressure, or measurement of volume by number of con­ densations ..._...,.......... ..,.........---.. ............... 51 Observations and measurements of gas wells in the lola quadrangle, by W. R. Crane............................................ -53 Measurements of static, or closed, pressure............ J........ 53 Measurements of the volume of gas wells...................... 55 Measurements of flow of gas in pipes........................... 59 Observations on methods of developing and utilizing oil and gas, by W. R. Crane............................................... 60 Methods of drilling............................................ 60 Cost and rate of drilling ...................................... 60 Systems of oil pumping........................................ 61 Distribution and control of gas supply ......................... 61 Portland cement .............:......................................... 63 Types of silicate cements....................................r...... 63 Puzzolan cement............................................. 63 Natural cement ............................................... 63 Portland cement ............................................. 64 Chemical composition of Portland cement.......................... 64 Physical properties........................................... 66 Kaw materials used in the manufacture of Portland cement......... 66 Siliceous and pure limestones.................................. 66 Marl and clay ................................................ 66 Chalky limestone and clay .................................... 66 Caustic-soda waste and clay................................... 67 Slag and limestone............................................ 67 Pure (hard) limestone and clay or shale. .................i..... 67 Cement materials in the lola quadrangle........................... 67 X Cement plants and processes of manufacture ....................... 67 lola Portland-cement plant.................................... 68 Kansas Portland-cement plant ................................ 69 Brick making........................................................ 69 Characteristics and properties of clays.............................. 69 Definition and composition of clays................................ 69 Classification of clays as to origin.................................. 69 Classification of clays as to uses........ ............................ 70 Clays in the lola quadrangle .......................................... 70 Condition of the brick industry ................................... 71 Brick plants atChanute....................................... 71 Brick plants at Humboldt..................................... 72 CONTENTS. 5 Mineral resources and their utilization, etc. Continued. Page. Brick making Continued. Clays in the lola quadrangle Continued. Brick plants at Tola........................... ................ 73 Brick plants at Laharpe....................................... 74 Coal, lead, and zinc.. .................................................. 74 Coal............................................................. 74 Lead and zinc.................................................... 75 Water supply .................................:..........-.-......... 75 Streams.......................................................... 75 Springs .... ^.....................................i................ 77 Wells............................................................ 77 Soils................................................................ 78 Origin of soils........................................ J........... 78 Classification of soils.............................................
Recommended publications
  • Proceedings Op the Twenty-Third Annual Meeting Op the Geological Society Op America, Held at Pittsburgh, Pennsylvania, December 21, 28, and 29, 1910
    BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 22, PP. 1-84, PLS. 1-6 M/SRCH 31, 1911 PROCEEDINGS OP THE TWENTY-THIRD ANNUAL MEETING OP THE GEOLOGICAL SOCIETY OP AMERICA, HELD AT PITTSBURGH, PENNSYLVANIA, DECEMBER 21, 28, AND 29, 1910. Edmund Otis Hovey, Secretary CONTENTS Page Session of Tuesday, December 27............................................................................. 2 Election of Auditing Committee....................................................................... 2 Election of officers................................................................................................ 2 Election of Fellows................................................................................................ 3 Election of Correspondents................................................................................. 3 Memoir of J. C. Ii. Laflamme (with bibliography) ; by John M. Clarke. 4 Memoir of William Harmon Niles; by George H. Barton....................... 8 Memoir of David Pearce Penhallow (with bibliography) ; by Alfred E. Barlow..................................................................................................................... 15 Memoir of William George Tight (with bibliography) ; by J. A. Bownocker.............................................................................................................. 19 Memoir of Robert Parr Whitfield (with bibliography by L. Hussa- kof) ; by John M. Clarke............................................................................... 22 Memoir of Thomas
    [Show full text]
  • Lithologic Description Checklist
    GY480 Field Geology Lithologic Description Checklist When describing outcrops you should attempt to determine the following at the exposure: 1. Rock name and/or Formation name (Granite, Cap Mt. Limestone member, etc.) 2. Color or color variations at outcrop (pink granite, vari-colored shale, etc.) 3. Mineralogy (estimate percentages if possible; try to distinguish between primary and secondary minerals) 4. texture: size, shape and arrangement of mineral grains (aphanitic, rhyolite porphyry, idioblastic, porphyroblastic, grain-supported, coarse sandstone, foliated granite, etc.). 5. Primary features: crossbeds, ripple marks, sole marks, igneous flow foliation, pillow basalt, vesicular basalt, etc.) Examples of well-written descriptions Sandstone (quartz arenite): white and very pale orange, weathers light brown and moderate reddish brown; very fine grained; subangular; well-sorted; laminated; locally cross-bedded; bedding thickness as much as a foot (30 cm), mostly covered with rubble; forms steep, rounded slope. Bolsa Quartzite. Granite, light gray or light pink, usually deeply weathered to light brown. Typically coarse- grained, containing large phenocrysts of pale-pink orthoclase up to 3 inches (7.6 cm) long. Coarse-grained groundmass consists of pale-pink orthoclase, chalky plagioclase (albite or andesine), quartz, and books of black biotite. Probably underlies diabase and sedimentary formations in most of the region. Ruin Granite. Schist, light to dark gray, weathers brown to greenish-brown. Comprised of a variety of types from coarse-grained quartz-sericite schist to fine-grained quartz-sericite-chlorite schist. Low- grade metamorphism greenschist facies; higher-grade occurs locally. Relict bedding of sedimentary protolith is generally recognizable in outcrop; plunging overturned tight to isoclinal folding is pervasive.
    [Show full text]
  • Chapter 8. Weathering, Sediment, & Soil
    Physical Geology, First University of Saskatchewan Edition is used under a CC BY-NC-SA 4.0 International License Read this book online at http://openpress.usask.ca/physicalgeology/ Chapter 8. Weathering, Sediment, & Soil Adapted by Karla Panchuk from Physical Geology by Steven Earle Figure 8.1 The Hoodoos, near Drumheller, Alberta, have formed from the differential weathering (weaker rock weathering faster than stronger rock) of sedimentary rock. Source: Steven Earle (2015) CC BY 4.0. Learning Objectives After reading this chapter and answering the review questions at the end, you should be able to: • Explain why rocks formed at depth in the crust are susceptible to weathering at the surface. • Describe the main processes of mechanical weathering, and the materials that are produced. • Describe the main processes of chemical weathering, and common chemical weathering products. • Explain the characteristics used to describe sediments, and what those characteristics can tell us about the origins of the sediments. • Discuss the relationships between weathering and soil formation, and the origins of soil horizons. • Describe and explain the distribution of Canadian soil types. • Explain how changing weathering rates affect the carbon cycle and the climate system. Chapter 8. Weathering, Sediment, & Soil 1 What Is Weathering? Weathering occurs when rock is exposed to the “weather” — to the forces and conditions that exist at Earth’s surface. Rocks that form deep within Earth experience relatively constant temperature, high pressure, have no contact with the atmosphere, and little or no interaction with moving water. Once overlying layers are eroded away and a rock is exposed at the surface, conditions change dramatically.
    [Show full text]
  • Geological Survey
    DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY ISTo. 162 WASHINGTON GOVERNMENT PRINTING OFFICE 1899 UNITED STATES GEOLOGICAL SUEVEY CHAKLES D. WALCOTT, DIRECTOR Olf NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINERALOGY FOR THE YEAR 1898 BY FRED BOUG-HTOISr WEEKS WASHINGTON GOVERNMENT PRINTING OFFICE 1899 CONTENTS, Page. Letter of transmittal.......................................... ........... 7 Introduction................................................................ 9 List of publications examined............................................... 11 Bibliography............................................................... 15 Classified key to the index .................................................. 107 Indiex....................................................................... 113 LETTER OF TRANSMITTAL. DEPARTMENT OF THE INTERIOR, UNITED STATES GEOLOGICAL SURVEY. Washington, D. C., June 30,1899. SIR: I have the honor to transmit herewith the manuscript of a Bibliography and Index o'f North American Geology, Paleontology, Petrology, and Mineralogy for the Year 1898, and to request that it be published as a bulletin of the Survey. Very respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, Director United States Geological Survey. 1 I .... v : BIBLIOGRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINERALOGY FOR THE YEAR 1898. ' By FEED BOUGHTON WEEKS. INTRODUCTION. The method of preparing and arranging the material of the Bibli­ ography and Index for 1898 is similar to that adopted for the previous publications 011 this subject (Bulletins Nos. 130,135,146,149, and 156). Several papers that should have been entered in the previous bulletins are here recorded, and the date of publication is given with each entry. Bibliography. The bibliography consists of full titles of separate papers, classified by authors, an abbreviated reference to the publica­ tion in which the paper is printed, and a brief summary of the con­ tents, each paper being numbered for index reference.
    [Show full text]
  • ROCK OUTCROP SYSTEM Ros12 Southern Floristic Region Southern Bedrock Outcrop Dry, Open Lichen-Dominated Plant Communities on Areas of Exposed Bedrock
    ROCK OUTCROP SYSTEM ROs12 Southern Floristic Region Southern Bedrock Outcrop Dry, open lichen-dominated plant communities on areas of exposed bedrock. Woody vegetation is sparse, and vascular plants are restricted to crevices, shallow soil deposits, and rainwater pools. Vegetation Structure & Composition Description is based on summary of vegetation plot data (relevés), plant species lists, and field notes from surveys of approximately 50 bedrock outcrops. • Lichen and bryophyte cover is high. On exposed bedrock, crustose and foliose lichens predominate. Species include Can- delariella vitellina, Lecanora muralis, Rhi- zocarpon disporum, Dimelaena oreina, Xanthoparmelia cumberlandia, Xanthopar- melia plittii, Acarospora americana, Physcia subtilis, and Dermatocarpon miniatum. On bedrock margins and along crevices, fruti- cose species such as Cladonia pyxidata are present with the more abundant crustose and foliose species. Common bryophytes on exposed rock include Schistidium and Grim- mia species, and, along crevices, Ceratodon purpureus, Weissia controversa, and Tortula species. Mosses often form carpets in shallow rainwater-collecting bedrock hollows. • Herbaceous plant cover is sparse to patchy (5–50%); characteristic species in crevices and areas with shallow soil (< 1in [3cm] deep), where plant biomass is low, include small-flowered fameflower (Talinum parviflorum), brittle prickly pear (Opuntia fragilis), rock spikemoss (Selaginella rupestris), rusty woodsia (Woodsia ilvensis), false pennyroyal (Isanthus brachiatus), slender knotweed
    [Show full text]
  • Chapter 9 Generally Have Cold Ocean Currents Flowing from the Checkpoint 9.1 Examine the Photos
    Geog 106LRS - Prof. Fischer Name ______Answer Key__ Chapter 9 generally have cold ocean currents flowing from the Checkpoint 9.1 Examine the photos. Both images poles toward the equator, of which the California show granite outcrops in the Sierra Nevada current is an example. Much of California is made of Mountains, California. Which outcrop contains accreted terranes from subduction zones that have pressure release cracks? Explain your existed along the coast over the last 200 million years choice. or so. a) Outcrop A b) Outcrop B Checkpoint 9.6 Weathering Analogies Matrix Many simple occurrences in our daily lives are Pressure release joints result in onion-skin-like similar to geologic processes. The following table exfoliation. contains some everyday events that you may have experienced. Match these actions to specific Checkpoint 9.2 Outcrops of granite are examined weathering processes. Complete the table by placing in California at similar elevations in the interior of the an “X” in the columns on the right-hand side where state more than 100 kilometers (63 miles) from the appropriate. For each characteristic in the Pacific Ocean and in outcrops along the coast. The left-hand column write in whether it is analogous granites have identical compositions and textures. On (similar) to physical, chemical, or biological the basis of the following information, which granite weathering. outcrop would weather most rapidly? Characteristic a) Outcrop A; located at coast, contains fractures Paint on house gradually disappears __________C spaced
    [Show full text]
  • A Walk Back in Time the Ruth Canstein Yablonsky Self-Guided Geology Trail
    The cross section below shows the rocks of the Watchung Reservation and surrounding area, revealing the relative positions of the lava flows that erupted in this region and the sedimentary rock layers between them. A Walk Back in Time The Ruth Canstein Yablonsky Self-Guided Geology Trail click here to view on a smart phone NOTES Trailside Nature & Science Center 452 New Providence Road, Mountainside, NJ A SERVICE OF THE UNION COUNTY BOARD OF UNION COUNTY (908) 789-3670 CHOSEN FREEHOLDERS We’re Connected to You! The Ruth Canstein Yablonsky Glossary basalt a fine-grained, dark-colored Mesozoic a span of geologic time from Self-Guided Geology Trail igneous rock. approximately 225 million years ago to 71 million years This booklet will act as a guide for a short hike to interpret the geological history bedrock solid rock found in the same area as it was formed. ago, and divided into of the Watchung Reservation. The trail is about one mile long, and all the stops smaller units called Triassic, described in this booklet are marked with corresponding numbers on the trail. beds layers of sedimentary rock. Jurassic and Cretaceous. conglomerate sedimentary rock made of oxidation a chemical reaction “Watchung” is a Lenape word meaning “high hill”. The Watchung Mountains have an rounded pebbles cemented combining with oxygen. elevation of about 600 feet above sea level. As you travel southeast, these high hills are the together by a mineral last rise before the gently rolling lowland that extends from Rt. 22 through appropriately substance (matrix) . Pangaea supercontinent that broke named towns like Westfield and Plainfield to the Jersey shore.
    [Show full text]
  • Global Geologic Maps Are Tectonic Speedometers— Rates of Rock Cycling from Area-Age Frequencies
    Global geologic maps are tectonic speedometers— Rates of rock cycling from area-age frequencies Bruce H. Wilkinson1†, Brandon J. McElroy2, Stephen E. Kesler3, Shanan E. Peters4, and Edward D. Rothman3 1Department of Earth Sciences, Syracuse University, Syracuse, New York 13244, USA 2Department of Geological Sciences, Jackson School of Geosciences, University of Texas, Austin, Texas 78712, USA 3Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan 48109, USA 4Department of Geology and Geophysics, University of Wisconsin, Madison, Wisconsin 53706, USA ABSTRACT the Earth’s surface, age-frequency distribu- lion years suggested by map age-frequencies tions for plutonic and metamorphic rocks are the same as would be anticipated on the Relations among ages and present areas of exhibit lognormal relations, with modes at basis of hundreds of published rates of ero- exposure of volcanic, sedimentary, plutonic, ca. 154 and 697 Ma, respectively. A dearth sional uplift and exhumation determined by and metamorphic rock units (lithosomes) of younger exposures of plutonic and meta- more conventional geochronometers. This record a complex interplay between depths morphic rocks refl ects the fact that these agreement suggests that geologic maps serve and rates of formation, rates of subsequent rock types form at depth, and some duration as effective deep-time speedometers for the tectonic subsidence and burial, and/or rates of tectonism is therefore required for their geologic rock cycle. of uplift and erosion. Thus, they potentially exposure. Increasing modal ages, from Qua- serve as effi cient deep-time geologic speed- ternary for volcanic and sedimentary succes- INTRODUCTION ometers, providing quantitative insight into sions, to early Mesozoic for intrusive rocks, rates of material transfer among the principal to Neoproterozoic for metamorphic rocks, Since the fi rst complete geologic map of Eng- rock reservoirs—processes central to the rock demonstrate that greater amounts of geologic land, Wales, and Scotland was scribed and pub- cycle.
    [Show full text]
  • Magnetic Minerals As Recorders of Weathering, Diagenesis, And
    Earth and Planetary Science Letters 452 (2016) 15–26 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl Magnetic minerals as recorders of weathering, diagenesis, and paleoclimate: A core–outcrop comparison of Paleocene–Eocene paleosols in the Bighorn Basin, WY, USA ∗ Daniel P. Maxbauer a,b, , Joshua M. Feinberg a,b, David L. Fox b, William C. Clyde c a Institute for Rock Magnetism, University of Minnesota, Minneapolis, MN, USA b Department of Earth Sciences, University of Minnesota, Minneapolis, MN, USA c Department of Earth Sciences, University of New Hampshire, Durham, NH, USA a r t i c l e i n f o a b s t r a c t Article history: Magnetic minerals in paleosols hold important clues to the environmental conditions in which the Received 17 February 2016 original soil formed. However, efforts to quantify parameters such as mean annual precipitation (MAP) Received in revised form 15 July 2016 using magnetic properties are still in their infancy. Here, we test the idea that diagenetic processes and Accepted 17 July 2016 surficial weathering affect the magnetic minerals preserved in paleosols, particularly in pre-Quaternary Available online 4 August 2016 systems that have received far less attention compared to more recent soils and paleosols. We evaluate Editor: H. Stoll the magnetic properties of non-loessic paleosols across the Paleocene–Eocene Thermal Maximum (a Keywords: short-term global warming episode that occurred at 55.5 Ma) in the Bighorn Basin, WY. We compare weathering data from nine paleosol layers sampled from outcrop, each of which has been exposed to surficial diagenesis weathering, to the equivalent paleosols sampled from drill core, all of which are preserved below environmental magnetism a pervasive surficial weathering front and are presumed to be unweathered.
    [Show full text]
  • Facies Analysis, Genetic Sequences, and Paleogeography of the Lower Part of the Minturn Formation (Middle Pennsylvanian), Southeastern Eagle Basin, Colorado
    Facies Analysis, Genetic Sequences, and Paleogeography of the Lower Part of the Minturn Formation (Middle Pennsylvanian), Southeastern Eagle Basin, Colorado U.S. GEOLOGICAL SURVEY BULLETIN 1 787-AA ^A2 Chapter AA Facies Analysis, Genetic Sequences, and Paleogeography of the Lower Part of the Minturn Formation (Middle Pennsylvanian), Southeastern Eagle Basin, Colorado By JOHN A. KARACHEWSKI A multidisciplinary approach to research studies of sedimentary rocks and their constituents and the evolution of sedimentary basins, both ancient and modern U.S. GEOLOGICAL SURVEY BULLETIN 1 787 EVOLUTION OF SEDIMENTARY BASINS UINTA AND PICEANCE BASINS U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government UNITED STATES GOVERNMENT PRINTING OFFICE: 1992 For sale by the Books and Open-File Report Sales U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Karachewski, John A. Facies analysis, genetic sequences, and paleogeography of the lower part of the Minturn Formation (Middle Pennsylvanian), Southeastern Eagle Basin, Colorado/ by John A. Karachewski. p. cm. (U.S. Geological Survey bulletin ; 1787) Evolution of sedimentary basins Uinta and Piceance basins ; ch. AA) Includes bibliographical references. Supt. of Docs, no.: I 19.3:1787 1. Sedimentation and deposition Colorado Eagle County. 2. Geology, Stratigraphic Pennsylvanian. 3. Geology, Stratigraphic Paleozoic. 4. Geology, Stratigraphic Colorado Eagle County. 5. Paleogeography Paleozoic. 6. Minturn Formation sedimentary basins Uinta and Piceance basins ; ch.
    [Show full text]
  • Bibliography and Index
    Bulletin No. 203. Series G, Miscellaneous, 23 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES .1). YVALCOTT, DIRECTOR BIBLIOGRAPHY AND INDEX FOR T I-I E Y E A. R 1 9 O 1 BY FRED BOUGHTON "WEEKS WASHINGTON - GOVERNMENT PRINTING OFFICE 1902 CONTENTS, Page. Letter of transmittal....................................................... 5 Introduction ......... 4 ................................................... 7 List of publications examined ............................................. 9 Bibliography ............................................................ 13 Addenda to bibliographies for previous years............................... 95 Classified key to the index ...........'.......... ............................ 97 Index ..................................................................... 103 LETTER OF TRANSM1TTAL. DEPARTMENT OF THE INTERIOR, UNITED STATES GEOLOGICAL SURVEY, Washington, D. 0., July % SIR: I have the honor to transmit herewith the manuscript of a Bibliography and Index of North American Geology, Paleontology, Petrology, and Mineralogy for the Year 1901, and to request that it be published as a Bulletin of the Survey. Yours respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, director United State* Geological Survey. BIBLIOGRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINERALOGY FOR THE YEAR 1901. By FRED BOUGHTON WEEKS. INTRODUCTION. The preparation and arrangement of the material of the Bibliog­ raphy and Index for 1901 is similar to that adopted for the previous publications.(Bulletins Nos. 130, 135, 146, 149, 156, 162, 172, 188, and 189). Several papers that should have been entered in the pre­ vious bulletins are here recorded, and the date of publication is given with each entry. Bibliography. The bibliography consists of full titles of separate papers, arranged alphabetically by authors' names, an abbreviated reference to the publication in which the paper is printed, and a brief description of the contents, each paper being numbered for index reference.
    [Show full text]
  • Mount Wrangell District, Alaska
    A, Economic Qeol y, 25 Rofeasional Paper No. 15 Series{ B, Dwmiptins Q&, 80 DEPARTMENT OF THE INTERIOR UNlTED S'l'hTES GEOLOGICAL SURVEY CHARLES U. \flALCOTT, I)IRECTOR THE MINERAL RESOURCES OF THE MOUNT WRANGELL DISTRICT, ALASKA BY WALTER C, MENDENHALL AND FRANK C, SCHRADER WASHINGTON GOVERNMENT PRINTING OFFICE 1903 .I MOUNT WRANGELL. VIFW t-keri frnm thi, Giivr,~nment im1 above To~is~iaBr~iloe 41 mles from tire sumtnit of tits maunin,~ I; NkDlNA RIVER BARS, Mnunt Drum in backgniuncl. Page . Introduction ................................................................................ 9 Copper ................................................................................... 13 Southern area ......................................................................... 13 Location ................................................................ ., ....... 13 Routes and trails ................................................................. 13 Geologic sketch .................................................................. 14 Nikolai greenstone ............................................................. 14 Chitistone limestone .......................................................... 14 Triassic shales and limestones ............................ .. .......... 15 Kennicott formation .......................................................... 15 Intrusive rocks ............................................................... 15 Copper occurrences ............................................................... 16 General statement ...........................................................
    [Show full text]