Automated Characterization of Yardangs Using Deep Convolutional Neural Networks
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Aeolian Processes and Landforms
Aeolian Processes and Landforms Ms. Deithra L. Archie, New Mexico State University Abstract I will present an overview of Aeolian processes and landforms on Mars. The overview will consist of two components. Component one is an overview of Aeolian processes and landforms on Earth and Mars, where the two planetary bodies are shown in Figures 1a and 1b respectively The second part of this paper will consist of image comparisons using satellite and MOC (Mars Orbiter Camera) images. Figure 1a Figure 1b Introduction Understanding the aeolian activity on the planet Mars and other planets begins with the study and knowledge of similar processes on Earth. Therefore, I will discuss the following: wind, particle entrainment and landforms found in the aeolian environment. This discussion will lead into my later discussion of the Martian sand seas and sand dunes. See Table 1 for a glossary of the terms used throughout this paper. In aeolian processes, wind transports and deposits particles of sediment. Aeolian features form in areas where wind is the primary source of erosion. The particles deposited are of sand, silt and clay size (see Table 2). The particles are entrained in by one of four processes. Creep is when a particle rolls or slides across the surface. Lift is when a particle rises off the surface due to the Bernoulli effect, the same mechanism which causes aircraft to rise. If the airflow is turbulent, larger particles are trajected by a process known as saltation. Finally, impact transport occurs which one particle strikes another causing the second particle to move. Erosional Landforms Wind eroded landforms are rarely preserved on the surface of the Earth except in arid regions. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
A Geomorphic Classification System
A Geomorphic Classification System U.S.D.A. Forest Service Geomorphology Working Group Haskins, Donald M.1, Correll, Cynthia S.2, Foster, Richard A.3, Chatoian, John M.4, Fincher, James M.5, Strenger, Steven 6, Keys, James E. Jr.7, Maxwell, James R.8 and King, Thomas 9 February 1998 Version 1.4 1 Forest Geologist, Shasta-Trinity National Forests, Pacific Southwest Region, Redding, CA; 2 Soil Scientist, Range Staff, Washington Office, Prineville, OR; 3 Area Soil Scientist, Chatham Area, Tongass National Forest, Alaska Region, Sitka, AK; 4 Regional Geologist, Pacific Southwest Region, San Francisco, CA; 5 Integrated Resource Inventory Program Manager, Alaska Region, Juneau, AK; 6 Supervisory Soil Scientist, Southwest Region, Albuquerque, NM; 7 Interagency Liaison for Washington Office ECOMAP Group, Southern Region, Atlanta, GA; 8 Water Program Leader, Rocky Mountain Region, Golden, CO; and 9 Geology Program Manager, Washington Office, Washington, DC. A Geomorphic Classification System 1 Table of Contents Abstract .......................................................................................................................................... 5 I. INTRODUCTION................................................................................................................. 6 History of Classification Efforts in the Forest Service ............................................................... 6 History of Development .............................................................................................................. 7 Goals -
Quaternary Geomorphic Processes and Landform Development in the Thar Desert of Rajasthan
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/302902544 Quaternary Geomorphic Processes and Landform Development in the Thar Desert of Rajasthan Chapter · January 2011 CITATIONS READS 6 4,293 1 author: Amal Kar Central Arid Zone Research Institute (CAZRI) 90 PUBLICATIONS 1,166 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Thar Desert Natural resources and their management View project Late Quaternary paleoclimate of the Thar Desert View project All content following this page was uploaded by Amal Kar on 11 May 2016. The user has requested enhancement of the downloaded file. acb publications Landforms Processes & Environment Management Kolkata, India Editor: S. Bandyopadhyay et al. [email protected] ISBN 81-87500-58-1 2011 (223-254) Quaternary Geomorphic Processes and Landform Development in the Thar Desert of Rajasthan Amal Kar1 Abstract: Evolution of landforms in the Thar Desert of Rajasthan is very much influenced by the exogenic and endogenic processes operating in the region during the Quaternary period. Studies have revealed that several fluctuations in climate between drier and wetter phases and periodic earth movements decided the type and intensity of geomorphic processes. The paper describes the broad sedimentation pattern in the desert, known facets of Quaternary climate and landform characteristics. It also discusses the influence of Quaternary climate change, neotectonism and human activities on landform evolution. Introduction The Thar, or the Great Indian Sand Desert, is situated in the arid western part of Rajasthan state in India and the adjoining sandy terrain of Pakistan. -
Formation and Evolution of Yardangs Activated by Late Pleistocene Tectonic Movement in Dunhuang, Gansu Province of China
Formation and evolution of yardangs activated by Late Pleistocene tectonic movement in Dunhuang, Gansu Province of China Yanjie Wang1,2, Fadong Wu1,∗, Xujiao Zhang1, Peng Zeng1, Pengfei Ma1, Yuping Song1 and Hao Chu1 1School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China. 2School of Tourism, Hebei University of Economics and Business, Shijiazhuang 050061, China. ∗Corresponding author. e-mail: [email protected] Developed in the Anxi-Dunhuang basin, the yardangs of Dunhuang (western China) are clearly affected by tectonic movement. Based on fieldwork, this study ascertained three levels of river terrace in the area for the first time. Through the analysis of river terraces formation and regional tectonic movement, the study ascertained that the river terraces were formed mainly by Late Pleistocene tectonic uplift, which had activated the evolution of yardangs in the study area. By electron spin resonance (ESR) dating and optically stimulated luminescence (OSL) dating, the starting time and periodicity of the evolution of the yardangs were determined. The river terraces designated T3, T2 and T1 began to evolve at 109.0∼98.5, 72.9∼66.84 and 53.2∼38.0 kaBP, respectively, which is the evidence of regional neotectonic movement. And, the formation of the yardangs was dominated by tectonic uplift during the prenatal stage and mainly by wind erosion in the following evolution, with relatively short stationary phases. This research focused on the determination of endogenic processes of yardangs formation, which would contribute to further understanding of yardangs formation from a geological perspective and promote further study of yardang landform. -
G Ro up of Sh Arp Y a R D a N G R Id G Es Sepa R A
BULL. GEOL. SOC. AM. VOL. 45, 1934, PL. Northeast of Rogers Dry Lake, Mohave Desert, California. GROUP OF SHARP YARDANG RIDGES SEPARATED BY TROUGHS Downloaded from http://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/45/1/159/3430339/BUL45_1-0159.pdf by guest on 24 September 2021 BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 45. PP. 159-166. PLS. 1-7 FEBRUARY 28, 1934 YARDANGS * BY ELIOT BLACKWELDER (Read before the Gordüleran Section of the Society, April 7 ,19SS) CONTENTS Page Yardangs defined...................................................................................................... 159 Some examples......................................................................................................... 160 Formation of yardangs and troughs....................................................................... 161 Limiting conditions................................................................................................. 163 Relative efficiency of wind as anerosional agent................................................... 164 References................................................................................................................. 165 YARDANGS DEFINED In this paper it is my purpose to describe certain features of con siderable size which are distinctive and seem clearly to be made by wind erosion. Although they have long been known to explorers of deserts, they have not received from geomorphologists the attention they deserve. The erosive activity of the wind has two aspects—which are -
Last Glacial Aeolian Landforms and Deposits in the Rhône Valley
Last Glacial aeolian landforms and deposits in the Rhône Valley (SE France): Spatial distribution and grain-size characterization Mathieu Bosq, Pascal Bertran, Jean-Philippe Degeai, Sebastian Kreutzer, Alain Queffelec, Olivier Moine, Eymeric Morin To cite this version: Mathieu Bosq, Pascal Bertran, Jean-Philippe Degeai, Sebastian Kreutzer, Alain Queffelec, et al.. Last Glacial aeolian landforms and deposits in the Rhône Valley (SE France): Spatial dis- tribution and grain-size characterization. Geomorphology, Elsevier, 2018, 318, pp.250 - 269. 10.1016/j.geomorph.2018.06.010. hal-01844757 HAL Id: hal-01844757 https://hal.archives-ouvertes.fr/hal-01844757 Submitted on 16 Jun 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Last Glacial aeolian landforms and deposits in the Rhône Valley (SE France): Spatial distribution and grain-size characterization Mathieu Bosqa, Pascal Bertrana,b, Jean-Philippe Degeaic, Sebastian Kreutzerd, Alain Queffeleca, Olivier Moinee, Eymeric Morinf,g a PACEA, UMR 5199 CNRS - Université Bordeaux, Bâtiment B8, allée Geoffroy -
Eolian Features in the Western Desert of Egypt and Some Applications to Mars
VOL. 84, NO. B14 JOURNAL OF GEOPHYSICAL RESEARCH DECEMBER 30, 1979 Eolian Features in the Western Desert of Egypt and Some Applications to Mars FAROUK EL-BAZ National Air and Space Museum, SmithsonianInstitution, Washington,D.C. 20560 C. S. BREED, M. J. GROLIER, AND J. F. MCCAULEY U.S. GeologicalSurvey, Flagstaff,Arizona 86001 Relations of landform types to wind regimes, bedrock composition, sediment supply, and topography are shown by field studiesand satellite photographsof the Western Desert of Egypt. This desert, which lies at the core of the largest hyperarid region on earth, provides analogs of Martian wind-formed fea- tures. These include sand dunes, alternating light and dark streaks,knob 'shadows,'and yardangs. Sur- face particleshave been segregatedby wind into deposits(dunes, sand sheets,and light streaks)that can be differentiated by their grain size distributions, surface shapes, and colors. Throughgoing sand of mostly fine to medium grain size is migrating southward in longitudinal dune belts and barchan chains whose long axes lie parallel to the prevailing northerly winds, but topographicvariations such as scarps and depressionsstrongly influence the zones of deposition and dune morphology. Sand from the longitu- dinal duneson the plains is commonly redistributedinto barchansin the depressions.These barchansare generally simple crescentsthat are morphologicallysimilar to many of the dunesseen on Viking orbiter pictures of the north polar sand sea on mars. Light streaksare depositional features consistingof dune belts and elongate sheetsof coarseto medium sand and granules.Intervening dark streaksare erosional features consistingof strips of desert-varnishedbedrock and lag gravel surfacesexposed between the sand deposits.The shape of both light and dark streaksis controlled by wind flow around topographic highs. -
Doi: 10.1103/Physreve.84.031304
ChinaXiv合作期刊 J Arid Land (2019) 11(5): 701–712 https://doi.org/ 10.1007/s40333-019-0108-4 Science Press Springer-Verlag Wind regime for long-ridge yardangs in the Qaidam Basin, Northwest China GAO Xuemin1,2,3*, DONG Zhibao4, DUAN Zhenghu1, LIU Min5, CUI Xujia5, LI Jiyan5,6 1 Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; 2 University of Chinese Academy of Sciences, Beijing 100049, China; 3 School of Tourism and Public Administration, Jinzhong University, Jinzhong 030619, China; 4 School of Geography and Tourism, Shaanxi Normal University, Xi'an 710062, China; 5 School of Geography Science, Taiyuan Normal University, Jinzhong 030619, China; 6 Key Laboratory of Education Ministry on Environment and Resources in Tibetan Plateau, Qinghai Normal University, Xining 810008, China Abstract: Yardangs are typical aeolian erosion landforms, which are attracting more and more attention of geomorphologists and geologists for their various morphology and enigmatic formation mechanisms. In order to clarify the aeolian environments that influence the development of long-ridge yardangs in the northwestern Qaidam Basin of China, the present research investigated the winds by installing wind observation tower in the field. We found that the sand-driving winds mainly blow from the north-northwest, northwest and north, and occur the most frequent in summer, because the high temperature increases atmospheric instability and leads to downward momentum transfer and active local convection during these months. The annual drift potential and the ratio of resultant drift potential indicate that the study area pertains to a high-energy wind environment and a narrow unimodal wind regime. -
Transverse Aeolian Ridges on Mars: First Results from Hirise Images
Geomorphology 121 (2010) 22–29 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Transverse Aeolian Ridges on Mars: First results from HiRISE images James R. Zimbelman ⁎ Center for Earth and Planetary Studies, MRC 315, National Air and Space Museum, Smithsonian Institution, Washington, D.C. 20013-7012, United States article info abstract Article history: Three images obtained by the High Resolution Imaging Science Experiment (HiRISE) were analyzed for the Received 11 July 2008 information they could provide regarding Transverse Aeolian Ridges (TARs) on Mars. TARs from five locations Received in revised form 23 February 2009 in a HiRISE image of the floor of Ius Chasma show remarkably symmetric (cross-sectional) profiles, with Accepted 26 May 2009 average slopes for the entire feature of ~15°; these results apply to TARs that span an order of magnitude in Available online 2 June 2009 wavelength and a factor of 6 in height. A HiRISE image of Gamboa impact crater in the northern lowlands shows low albedo sand patches b2 m high that are covered with sand ripples, surrounded by larger TAR-like Keywords: fi Sand ripples that are very similar in pro le to surveyed granule ripples on Earth. TARs in a HiRISE image from Terra Dune Sirenum, in the cratered southern highlands, are comparable in height to those in Ius Chasma, but many have Ripple tapered extensions that are more consistent with them being erosional remnants rather than the result of Granule ripple extension of the TAR by deposition from the tapered end. The new observations generally support a reversing Topography transverse dune origin for TARs with heights ≥1 m, and a granule ripple origin for TAR-like ripples with Transverse dune heights ≤0.5 m. -
Megaripple Stripes
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2019-04-25 Megaripple Stripes Gough, Tyler Robert Gough, T. R. (2019). Megaripple Stripes (Unpublished master's thesis). University of Calgary, Calgary, AB. http://hdl.handle.net/1880/110217 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Megaripple Stripes by Tyler Robert Gough A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE GRADUATE PROGRAM IN GEOGRAPHY CALGARY, ALBERTA APRIL, 2019 © Tyler Robert Gough 2019 ii Abstract This thesis incorporates field measurements, satellite imagery, and numerical modeling to explain the formation and evolution of a poorly understood and relatively undocumented longitudinal aeolian bedform pattern. The pattern consists of alternating streamwise corridors of megaripples separated by corridors containing smaller bedforms. This pattern, referred to herein as megaripple stripes, is observed at sites on Earth and Mars. Measurements from satellite imagery indicate a strong positive relation between the crosswind and downwind wavelengths of megaripple corridors. Field measurements of stripe morphology and grain size indicate a consistent pattern whereby the surface texture of the megaripple corridors is coarser than the intervening corridors of smaller bedforms. -
Alphabetical Glossary of Geomorphology
International Association of Geomorphologists Association Internationale des Géomorphologues ALPHABETICAL GLOSSARY OF GEOMORPHOLOGY Version 1.0 Prepared for the IAG by Andrew Goudie, July 2014 Suggestions for corrections and additions should be sent to [email protected] Abime A vertical shaft in karstic (limestone) areas Ablation The wasting and removal of material from a rock surface by weathering and erosion, or more specifically from a glacier surface by melting, erosion or calving Ablation till Glacial debris deposited when a glacier melts away Abrasion The mechanical wearing down, scraping, or grinding away of a rock surface by friction, ensuing from collision between particles during their transport in wind, ice, running water, waves or gravity. It is sometimes termed corrosion Abrasion notch An elongated cliff-base hollow (typically 1-2 m high and up to 3m recessed) cut out by abrasion, usually where breaking waves are armed with rock fragments Abrasion platform A smooth, seaward-sloping surface formed by abrasion, extending across a rocky shore and often continuing below low tide level as a broad, very gently sloping surface (plain of marine erosion) formed by long-continued abrasion Abrasion ramp A smooth, seaward-sloping segment formed by abrasion on a rocky shore, usually a few meters wide, close to the cliff base Abyss Either a deep part of the ocean or a ravine or deep gorge Abyssal hill A small hill that rises from the floor of an abyssal plain. They are the most abundant geomorphic structures on the planet Earth, covering more than 30% of the ocean floors Abyssal plain An underwater plain on the deep ocean floor, usually found at depths between 3000 and 6000 m.