Riverine Analysis
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Interpretations of Gravity Anomalies at Olympus Mons, Mars: Intrusions, Impact Basins, and Troughs
Lunar and Planetary Science XXXIII (2002) 2024.pdf INTERPRETATIONS OF GRAVITY ANOMALIES AT OLYMPUS MONS, MARS: INTRUSIONS, IMPACT BASINS, AND TROUGHS. P. J. McGovern, Lunar and Planetary Institute, Houston TX 77058-1113, USA, ([email protected]). Summary. New high-resolution gravity and topography We model the response of the lithosphere to topographic loads data from the Mars Global Surveyor (MGS) mission allow a re- via a thin spherical-shell flexure formulation [9, 12], obtain- ¡g examination of compensation and subsurface structure models ing a model Bouguer gravity anomaly ( bÑ ). The resid- ¡g ¡g ¡g bÓ bÑ in the vicinity of Olympus Mons. ual Bouguer anomaly bÖ (equal to - ) can be Introduction. Olympus Mons is a shield volcano of enor- mapped to topographic relief on a subsurface density interface, using a downward-continuation filter [11]. To account for the mous height (> 20 km) and lateral extent (600-800 km), lo- cated northwest of the Tharsis rise. A scarp with height up presence of a buried basin, we expand the topography of a hole Ö h h ¼ ¼ to 10 km defines the base of the edifice. Lobes of material with radius and depth into spherical harmonics iÐÑ up h with blocky to lineated morphology surround the edifice [1-2]. to degree and order 60. We treat iÐÑ as the initial surface re- Such deposits, known as the Olympus Mons aureole deposits lief, which is compensated by initial relief on the crust mantle =´ µh c Ñ c (hereinafter abbreviated as OMAD), are of greatest extent to boundary of magnitude iÐÑ . These interfaces the north and west of the edifice. -
Sinuous Ridges in Chukhung Crater, Tempe Terra, Mars: Implications for Fluvial, Glacial, and Glaciofluvial Activity Frances E.G
Sinuous ridges in Chukhung crater, Tempe Terra, Mars: Implications for fluvial, glacial, and glaciofluvial activity Frances E.G. Butcher, Matthew Balme, Susan Conway, Colman Gallagher, Neil Arnold, Robert Storrar, Stephen Lewis, Axel Hagermann, Joel Davis To cite this version: Frances E.G. Butcher, Matthew Balme, Susan Conway, Colman Gallagher, Neil Arnold, et al.. Sinuous ridges in Chukhung crater, Tempe Terra, Mars: Implications for fluvial, glacial, and glaciofluvial activity. Icarus, Elsevier, 2021, 10.1016/j.icarus.2020.114131. hal-02958862 HAL Id: hal-02958862 https://hal.archives-ouvertes.fr/hal-02958862 Submitted on 6 Oct 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. 1 Sinuous Ridges in Chukhung Crater, Tempe Terra, Mars: 2 Implications for Fluvial, Glacial, and Glaciofluvial Activity. 3 Frances E. G. Butcher1,2, Matthew R. Balme1, Susan J. Conway3, Colman Gallagher4,5, Neil 4 S. Arnold6, Robert D. Storrar7, Stephen R. Lewis1, Axel Hagermann8, Joel M. Davis9. 5 1. School of Physical Sciences, The Open University, Walton Hall, Milton Keynes, MK7 6 6AA, UK. 7 2. Current address: Department of Geography, The University of Sheffield, Sheffield, S10 8 2TN, UK ([email protected]). -
Sinuous Ridges in Chukhung Crater, Tempe Terra, Mars: Implications for Fluvial, Glacial, and Glaciofluvial Activity
This is a repository copy of Sinuous ridges in Chukhung crater, Tempe Terra, Mars: Implications for fluvial, glacial, and glaciofluvial activity. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/166644/ Version: Published Version Article: Butcher, F.E.G. orcid.org/0000-0002-5392-7286, Balme, M.R., Conway, S.J. et al. (6 more authors) (2021) Sinuous ridges in Chukhung crater, Tempe Terra, Mars: Implications for fluvial, glacial, and glaciofluvial activity. Icarus, 357. 114131. ISSN 0019-1035 https://doi.org/10.1016/j.icarus.2020.114131 Reuse This article is distributed under the terms of the Creative Commons Attribution (CC BY) licence. This licence allows you to distribute, remix, tweak, and build upon the work, even commercially, as long as you credit the authors for the original work. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Journal Pre-proof Sinuous ridges in Chukhung crater, Tempe Terra, Mars: Implications for fluvial, glacial, and glaciofluvial activity Frances E.G. Butcher, Matthew R. Balme, Susan J. Conway, Colman Gallagher, Neil S. Arnold, Robert D. Storrar, Stephen R. Lewis, Axel Hagermann, Joel M. Davis PII: S0019-1035(20)30473-5 DOI: https://doi.org/10.1016/j.icarus.2020.114131 Reference: YICAR 114131 To appear in: Icarus Received date: 2 June 2020 Revised date: 19 August 2020 Accepted date: 28 September 2020 Please cite this article as: F.E.G. -
Information to Users
RELATIVE AGES AND THE GEOLOGIC EVOLUTION OF MARTIAN TERRAIN UNITS (MARS, CRATERS). Item Type text; Dissertation-Reproduction (electronic) Authors BARLOW, NADINE GAIL. Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 06/10/2021 23:02:22 Link to Item http://hdl.handle.net/10150/184013 INFORMATION TO USERS While the most advanced technology has been used to photograph and reproduce this manuscript, the quality of the reproduction is heavily dependent upon the quality of the material submitted. For example: • Manuscript pages may have indistinct print. In such cases, the best available copy has been filmed. o Manuscripts may not always be complete. In such cases, a note will indicate that it is not possible to obtain missing pages. • Copyrighted material may have been removed from the manuscript. In such cases, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, and charts) are photographed by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps. Each oversize page is also filmed as one exposure and is available, for an additional charge, as a standard 35mm slide or as a 17"x 23" black and white photographic print. Most photographs reproduce acceptably on positive microfilm or microfiche but lack the clarity on xerographic copies made from the microfilm. -
Modeling and Mapping of the Structural Deformation of Large Impact Craters on the Moon and Mercury
MODELING AND MAPPING OF THE STRUCTURAL DEFORMATION OF LARGE IMPACT CRATERS ON THE MOON AND MERCURY by JEFFREY A. BALCERSKI Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Earth, Environmental, and Planetary Sciences CASE WESTERN RESERVE UNIVERSITY August, 2015 CASE WESTERN RESERVE UNIVERSITY SCHOOL OF GRADUATE STUDIES We hereby approve the thesis/dissertation of Jeffrey A. Balcerski candidate for the degree of Doctor of Philosophy Committee Chair Steven A. Hauck, II James A. Van Orman Ralph P. Harvey Xiong Yu June 1, 2015 *we also certify that written approval has been obtained for any proprietary material contained therein ~ i ~ Dedicated to Marie, for her love, strength, and faith ~ ii ~ Table of Contents 1. Introduction ............................................................................................................1 2. Tilted Crater Floors as Records of Mercury’s Surface Deformation .....................4 2.1 Introduction ..............................................................................................5 2.2 Craters and Global Tilt Meters ................................................................8 2.3 Measurement Process...............................................................................12 2.3.1 Visual Pre-selection of Candidate Craters ................................13 2.3.2 Inspection and Inclusion/Exclusion of Altimetric Profiles .......14 2.3.3 Trend Fitting of Crater Floor Topography ................................16 2.4 Northern -
Western Upper Peninsula Citizens Advisory Council Division Reports
Western Upper Peninsula Citizen Advisory Council DNR Division Reports Date of Production: July 2017 This documentation is provided by Michigan DNR staff as a supplement to verbal reports that will be distributed to the Western UPCAC at the July 19th meeting in Harris, MI. Upper Peninsula Regional Coordinator Update – Stacy Haughey, UP Regional Coordinator DNR Public Meetings July 13 Forestry Compartment Review-Baraga Unit, DNR Baraga Office, 9:00am July 13 Natural Resources Commission UP Meeting, Lansing July 20 Western UP Citizens’ Advisory Council Meeting, Harris, 5:00pm Central/6:00pm Eastern August 2 Forestry Open House-Escanaba Unit, Stephenson Field Office, 4:00pm Eastern August 10 Natural Resources Commission Meeting, Jackson August 15 Michigan Iron Industry Museum Advisory Board Meeting, Negaunee, 3:00pm August 16 Forestry Compartment Review-Escanaba Unit, Escanaba State Office Building, 9:00am DNR Pocket Park – UP State Fair in Escanaba – August 14 through August 20, 2017 WE NEED YOU! It’s never too early to start thinking about volunteering at the DNR Pocket Park in Escanaba during the week of the UP State Fair. Please consider volunteering with your group or family member(s) and help to teach a young girl or boy to catch a fish or shoot a pellet gun. Over 200 slots to fill! Create and nurture a new generation of young UP sportspersons! Call or email Kristi Dahlstrom ([email protected] / 906-226- 1331) or Jo Ann Alexander ([email protected] / 906-786-2351) to reserve your volunteer slot NOW! U.P. State Park & State Sponsored Activities July 15 Baraga State Park-Kayaking 101 and 202 July 16 Indian Lake State Park-Street Chalk Art July 18 Michigan Iron Industry Museum-Magnificent Mansions and Courtly Cottages in the U.P. -
The Impact Origin and Evolution of Chryse Planitia on Mars Revealed by Buried Craters
ARTICLE https://doi.org/10.1038/s41467-019-12162-0 OPEN The impact origin and evolution of Chryse Planitia on Mars revealed by buried craters Lu Pan 1, Cathy Quantin-Nataf1, Sylvain Breton1 & Chloé Michaut 1 Large impacts are one of the most important processes shaping a planet’s surface. On Mars, the early formation of the Martian crust and the lack of large impact basins (only four unambiguously identified: Hellas, Argyre, Utopia, and Isidis) indicates that a large part of ’ 1234567890():,; early records of Mars impact history is missing. Here we show, in Chryse Planitia, the scarcity of buried impact craters in a near-circular area could be explained by a pre-existing topographic depression with more intense resurfacing. Spatially correlated with positive Bouguer anomaly, this near-circular region with a diameter of ~1090 km likely originated from an impact. This proposed large impact basin must have been quickly relaxed or buried after its formation more than 4.0 billion years ago and heavily modified by subsequent resurfacing events. We anticipate our study to open a new window to unravelling the buried records of early Martian bombardment record. 1 Université de Lyon, Université Claude Bernard Lyon 1, ENS de Lyon, CNRS, UMR 5276 Laboratoire de Géologie de Lyon -Terre, Planètes, Environnement, 69622 Villeurbanne, France. Correspondence and requests for materials should be addressed to L.P. (email: [email protected]) NATURE COMMUNICATIONS | (2019) 10:4257 | https://doi.org/10.1038/s41467-019-12162-0 | www.nature.com/naturecommunications 1 ARTICLE NATURE COMMUNICATIONS | https://doi.org/10.1038/s41467-019-12162-0 arge basin-forming impacts significantly modified planetary could be the original Chryse impact basin, which subsequently surfaces and crusts, especially in the first billion years of underwent heavy degradation. -
Ricane Magazines
■' ■■ A;, PAGE TWENTl >»> WEDNESDAY.'SEPTEMBER 7, 1969 iffiattrlTPBffr I fm lb A vence Didiy Nat Preaa Ron Hie Weather for tlw WMfe Bated ronMoot a t D.E8. WaattMa BoMM «iDM4tii.isar . rU r mad wvm taalgU. l.aw dt 13,125 X t« as. Fridor OMMttlt wony, w ant Hemlwr o< ttaa Aadlt «6yh a fn r Mattered ehowera Uk»- Bonon of Obwnlattoa Ijr. Hifk la Ste. M aneheaUr^A City of Village Charm VOL. LXXIX. NO. 289 iCTWENTY PAGES) MANCHESTER, CONN., THURSDAY, SEPTEMBER 8, 1960 (OlaMlOed AdvertlBlnc on Page 18) PRICJ^ FIVB CENTS Blasts VN, Belgium Second Group from the pages of the Plans Look at nation^s leading fashion Security Check ricane magazines... and our very .Washington, Sept. 8 (4^--- A second congressional com mittee is Goins to look into own second floor sportswear tJie defection of two U.S. code clerks; , Leopoldville. The C ongo.f^ion* “ "“ rntag the U.N. will A special 5-man subcon^nittee departrnent!... be Ukeh shortly.. of the House Armed Services Com Sept. 8 <i<P)-7-Preinier Patrice 11 16 announcement was issued mittee was formed, yesterday to X Lumumba went before an in the wake of the national assem check on how the Pentagon and angry Senate today to defend bly’s action yesterday voiding at Central Intelilgence Agency SWEATERS FOR '60 tempts by the conservative presi <CIA) ’’rsofult, screen, re-screen Trainmen Ask his, government and two dent and the left-leaning premier Full Force hours later they were cheek and clear their personnel.” to fire each other from their Jobs. -
Seeds and Supplies 2021
FEDCO 2021 Seeds and Supplies Where Is erthing Ordering Instructions page 160 Order Forms pages 161-166 Complete Index inside back cover begin on page Welcome to Fedco’s rd ear Vegetable Seeds 5 “May you live in interesting times”… redux. Herb Seeds 79 How eerily prescient it was to invoke that adage a year Flower Seeds 86 ago—and then to experience it play out as both a curse and a blessing. Onion Sets & Plants 110 So much has shifted in a year. In our last catalog we Ginger, turmeric, sweet potato 111 brought you interviews with innovators in agriculture whose Potatoes 111 wisdom spoke to a more inclusive, regenerative and Farm Seed / Cover Crops 118 holistic future. Those visions, with all the excitement and challenge they bring, are rapidly taking hold and Soil Amendments 124 rooting in the disturbance of 2020. Pest Control 134 We see it all around us: my son’s cul-de-sac Tools 140 organized to grow food together. Neighborhoods Books 151 started seed banks. Signs sprang up in towns for Planting Guides & Lists: Give & Take tables for garden produce, to share what you can and take what you need. Winona La Duke, in Vegetable Chart 77 her (online) Common Ground Fair keynote, stressed the Botanical Index 78 building of local infrastructures. If we look outside the Herb Chart 79 strident newsfeed, we see new structures evolving from Flower Chart 86 common values. Seed Longevity Charts 92, 106 So in this year’s interviews we take a closer look at Organic Variety List 104 what’s unfolding. -
Lithospheric Structure and Tectonics at Isidis Planitia, Mars ∗ J
Icarus 201 (2009) 528–539 Contents lists available at ScienceDirect Icarus www.elsevier.com/locate/icarus Lithospheric structure and tectonics at Isidis Planitia, Mars ∗ J. Andreas Ritzer ,StevenA.Hauck,II Department of Geological Sciences, Case Western Reserve University, 112 A.W. Smith Bldg., 10900 Euclid Ave, Cleveland, OH 44106-7216, United States article info abstract Article history: We characterize the lithospheric structure of Isidis Planitia on Mars by analyzing Mars Global Surveyor Received 2 May 2008 and Mars Odyssey gravity and topography data using a flexural model of a thin elastic shell including Revised 3 December 2008 bending and membrane stresses. Isidis Planitia is a circular, relatively flat plain formed near the end Accepted 21 January 2009 of the Early Noachian, at the edge of the highlands–lowlands boundary and the site of a large free- Availableonline13February2009 air gravity anomaly, features consistent with modification and filling of an impact basin. Our results −3 Keywords: suggest that the bulk density of the fill material inside Isidis must be more than 2600 kg m and Mars higher densities are probable. A comparison of the faulting observed at Nili Fossae to the predicted zone Tectonics of extensional strain northwest of Isidis constrains the thickness of the elastic lithosphere to be 100– Geophysics 180 km thick beneath the basin at the time of loading. We also find that loads outside of the basin play a significant role in the interpretation of the tectonics; simplified models tend to overestimate the − lithospheric thickness. We place relatively narrow bounds on the thermal gradient (3.4–6.5 K km 1)and − heat flux (13.6–26 mW m 2)atIsidisatthetimeofloading. -
FULLTEXT01.Pdf
Implementing the Selfoss declaration Recommendations to Nordic forestry TemaNord 2010:554 Implementing the Selfoss declaration Recommendations to Nordic forestry TemaNord 2010:554 © Nordic Council of Ministers, Copenhagen 2010 ISBN 978-92-893-2085-6 Print: Kailow Express ApS Cover photo: Image Select Copies: 200 Printed on environmentally friendly paper This publication can be ordered on www.norden.org/order. Other Nordic publications are available at www.norden.org/publications This publication has been published with financial support by the Nordic Council of Ministers. But the contents of this publication do not necessarily reflect the views, policies or recommendations of the Nordic Council of Ministers. Printed in Denmark Nordic Council of Ministers Nordic Council Ved Stranden 18 Ved Stranden 18 DK-1061 København K DK-1061 København K Phone (+45) 3396 0200 Phone (+45) 3396 0400 Fax (+45) 3396 0202 Fax (+45) 3311 1870 www.norden.org Nordic co-operation Nordic co-operation is one of the world’s most extensive forms of regional collaboration, involving Denmark, Finland, Iceland, Norway, Sweden, and three autonomous areas: the Faroe Islands, Green- land, and Åland. Nordic co-operation has firm traditions in politics, the economy, and culture. It plays an important role in European and international collaboration, and aims at creating a strong Nordic community in a strong Europe. Nordic co-operation seeks to safeguard Nordic and regional interests and principles in the global community. Common Nordic values help the region solidify its position as one of the world’s most innovative and competitive. Content 1. Introduction .................................................................................................................... 7 The Selfoss Declaration on sustainable forestry ................................................................... -
"G" S Circle 243 Elrod Dr Goose Creek Sc 29445 $5.34
Unclaimed/Abandoned Property FullName Address City State Zip Amount "G" S CIRCLE 243 ELROD DR GOOSE CREEK SC 29445 $5.34 & D BC C/O MICHAEL A DEHLENDORF 2300 COMMONWEALTH PARK N COLUMBUS OH 43209 $94.95 & D CUMMINGS 4245 MW 1020 FOXCROFT RD GRAND ISLAND NY 14072 $19.54 & F BARNETT PO BOX 838 ANDERSON SC 29622 $44.16 & H COLEMAN PO BOX 185 PAMPLICO SC 29583 $1.77 & H FARM 827 SAVANNAH HWY CHARLESTON SC 29407 $158.85 & H HATCHER PO BOX 35 JOHNS ISLAND SC 29457 $5.25 & MCMILLAN MIDDLETON C/O MIDDLETON/MCMILLAN 227 W TRADE ST STE 2250 CHARLOTTE NC 28202 $123.69 & S COLLINS RT 8 BOX 178 SUMMERVILLE SC 29483 $59.17 & S RAST RT 1 BOX 441 99999 $9.07 127 BLUE HERON POND LP 28 ANACAPA ST STE B SANTA BARBARA CA 93101 $3.08 176 JUNKYARD 1514 STATE RD SUMMERVILLE SC 29483 $8.21 263 RECORDS INC 2680 TILLMAN ST N CHARLESTON SC 29405 $1.75 3 E COMPANY INC PO BOX 1148 GOOSE CREEK SC 29445 $91.73 A & M BROKERAGE 214 CAMPBELL RD RIDGEVILLE SC 29472 $6.59 A B ALEXANDER JR 46 LAKE FOREST DR SPARTANBURG SC 29302 $36.46 A B SOLOMON 1 POSTON RD CHARLESTON SC 29407 $43.38 A C CARSON 55 SURFSONG RD JOHNS ISLAND SC 29455 $96.12 A C CHANDLER 256 CANNON TRAIL RD LEXINGTON SC 29073 $76.19 A C DEHAY RT 1 BOX 13 99999 $0.02 A C FLOOD C/O NORMA F HANCOCK 1604 BOONE HALL DR CHARLESTON SC 29407 $85.63 A C THOMPSON PO BOX 47 NEW YORK NY 10047 $47.55 A D WARNER ACCOUNT FOR 437 GOLFSHORE 26 E RIDGEWAY DR CENTERVILLE OH 45459 $43.35 A E JOHNSON PO BOX 1234 % BECI MONCKS CORNER SC 29461 $0.43 A E KNIGHT RT 1 BOX 661 99999 $18.00 A E MARTIN 24 PHANTOM DR DAYTON OH 45431 $50.95