Comparing Geomorphometric Pattern Recognition Methods for Semi-Automated
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Draft Final Remedial Investigation / Feasibility Study (Ri/Fs)
Snperfondi RMQ SITE: DRAFT FINAL PKEAK; REMEDIAL VOLUME 1 OF 4 - TEXT REMEDIAL INVESTIGATION/FEASIBILITY STUDY NEW HAMPSHIRE PLATING COMPANY MERRIMACK, NEW HAMPSHIRE For U.S. Environmental Protection Agency By Halliburton NUS Corporation and Raytheon Engineers & Constructors, Inc. EPA Work Assignment No. 33-1LG1 EPA Contract No. 68-W8-0117 HNUS Project No. 0772 May 1996 Halliburton NTJS CORPORATION W94619DF DRAFT FINAL REMEDIAL INVESTIGATION REPORT VOLUME 1 OF 4 - TEXT REMEDIAL INVESTIGATION/FEASIBILITY STUDY NEW HAMPSHIRE PLATING COMPANY MERRIMACK, NEW HAMPSHIRE For U.S. Environmental Protection Agency By Halliburton NUS Corporation and Raytheon Engineers & Constructors, Inc. EPA Work Assignment No. 33-1LG1 EPA Contract No. 68-W8-0117 HNUS Project No. 0772 May 1996 Marilyn M. Wade, P.E. George D(7Gardner, P.E. Project Manager Program Manager DRAFT FINAL TABLE OF CONTENTS VOLUME 1 - TEXT DRAFT FINAL REMEDIAL INVESTIGATION REPORT NEW HAMPSHIRE PLATING COMPANY SITE MERRIMACK, NEW HAMPSHIRE SECTION PAGE E.O EXECUTIVE SUMMARY ES-1 1.0 INTRODUCTION 1-1 1.1 Site and Study Area Background 1-2 1.2 NHPC Site History 1-3 1.3 Report Organization 1-4 2.0 STUDY AREA INVESTIGATION 2-1 2.1 Previous Investigations 2-1 2.1.1 Peck Environmental Laboratory ,Inc 2-1 2.1.2 Wehran Engineerin g 2-2 2.1.3 New Hampshire Department of Environmental Services (NHDES) 2-3 2.1.4 Removal Actio n- U.S. EPA Emergency Response Team (ERT) 2-4 2.1.5 Wetlan dInvestigation 2-5 2.1.6 Technical Assistance Groundwater Samplin g 2-6 2.1.7 Non-Time-Critical Removal Action 2-7 2.1.8 Previous Investigation son Properties Abutting the NHPC Site 2-9 2.1.8.1 Magnum Leasing and Mortgage Company . -
RECREATION GUIDE 2021 1 Your BUTTE FAMILY IS IMPORTANT to Our BUTTE FAMILY
2021 Kids Summer Fun Events Pg.27 Pg.8-9 Brought to you by BUTTE RECREATION GUIDE 2021 1 Your BUTTE FAMILY IS IMPORTANT TO our BUTTE FAMILY townpump.com 2 BUTTE RECREATION GUIDE 2021 BUTTE RECREATION GUIDE 2021 3 OUR MISSION e Butte-Silver Bow Parks and Recreation Department is committed to improving our community’s health, stability, beauty, and quality of life by providing outstanding parks, trails, recreational facilities and leisure opportunities for all of our citizens. Butte-Silver Bow Parks & Recreation at a glance: • More than two dozen parks (many with pavilions that can be reserved), numerous playgrounds, a 9 hole regulation golf course, a par-3 golf course, a clubhouse with golf simulators, two disc golf courses, a splash pad, and a wading pool • Ridge Waters: A family water park featuring two water slides, a lazy river, a zero depth entry children’s area, a climbing wall, a diving board, swimming lanes, rentable cabanas, and a concession stand • A new destination playground at Stodden Park • An extensive urban and rural trail system • ompson Park: e only dually managed municipal/National Forest Service park in the nation • Adult and youth programming, which include: volleyball, softball and pickleball and more • Two historic mine yards that are now event facilities • Community-wide special events CONTENTS Parks & Recreation Fast Facts…Page 6 Butte Arborist…Page 7 Ridge Waters…Page 8 We’re on the web! Stodden Park…Page 10 butteparksandrec.com ridgewaters.com Popular Urban Parks…Page 11 highlandviewgolf.com Recreational Facilities…Page 16 Find us on Facebook, Twitter and Instagram! Mine Yards…Page 18 Rural Parks & Recreation Near Butte…Page 20 Thompson Park Map…Page 22 Butte Urban Map…Page 23 @ButteParks @ButteSilverBow @ButteParksandRec Highland View Golf Course…Page 25 Summer Fun Youth Events…Page 27 Regional Outdoor Opportunities… On the cover: Page 29 Cyclist in Thompson Park. -
A Brief Guide
CHAPTER 1 Geomorphometry: A Brief Guide R.J. Pike, I.S. Evans and T. Hengl basic definitions · the land surface · land-surface parameters and objects · digital elevation models (DEMs) · basic principles of geomorphometry from a GIS perspective · inputs/outputs, data structures & algorithms · history of geomorphometry · geomorphometry today · data set used in this book 1. WHAT IS GEOMORPHOMETRY? Geomorphometry is the science of quantitative land-surface analysis (Pike, 1995, 2000a; Rasemann et al., 2004). It is a modern, analytical-cartographic approach to rep- resenting bare-earth topography by the computer manipulation of terrain height (Tobler, 1976, 2000). Geomorphometry is an interdisciplinary field that has evolved from mathematics, the Earth sciences, and — most recently — computer science (Figure 1). Although geomorphometry1 has been regarded as an activity within more established fields, ranging from geography and geomorphology to soil sci- ence and military engineering, it is no longer just a collection of numerical tech- niques but a discipline in its own right (Pike, 1995). It is well to keep in mind the two overarching modes of geomorphometric analysis first distinguished by Evans (1972): specific, addressing discrete surface features (i.e. landforms), and general, treating the continuous land surface. The morphometry of landforms per se, by or without the use of digital data, is more correctly considered part of quantitative geomorphology (Thorn, 1988; Scheidegger, 1991; Leopold et al., 1995; Rhoads and Thorn, 1996). Geomorphometry in this book is primarily the computer characterisation and analysis of continuous topography. A fine-scale counterpart of geomorphometry in manufacturing is industrial surface metrology (Thomas, 1999; Pike, 2000b). The ground beneath our feet is universally understood to be the interface be- tween soil or bare rock and the atmosphere. -
Evaporation from Salty Lagoons (Case Study: Qattara Depression)
The British University in Egypt BUE Scholar Civil Engineering Engineering Spring 4-2017 Evaporation from Salty Lagoons (Case Study: Qattara Depression) Mohamed Abdelhamid Eizeldin Dr. [email protected] Heba Abdelazim M.Sc Sherif Eldidy Prof. Cairo University Follow this and additional works at: https://buescholar.bue.edu.eg/civil_eng Part of the Civil Engineering Commons, and the Hydraulic Engineering Commons Recommended Citation Eizeldin, Mohamed Abdelhamid Dr.; Abdelazim, Heba M.Sc; and Eldidy, Sherif Prof., "Evaporation from Salty Lagoons (Case Study: Qattara Depression)" (2017). Civil Engineering. 7. https://buescholar.bue.edu.eg/civil_eng/7 This Conference Proceeding is brought to you for free and open access by the Engineering at BUE Scholar. It has been accepted for inclusion in Civil Engineering by an authorized administrator of BUE Scholar. For more information, please contact [email protected]. Al-Azhar University Civil Engineering Research Magazine (CERM) Vol. (39) No. (2) April, 2017 Evaporation from Salty Lagoons (Case Study: Qattara Depression) Abdel Azeem, H.S1, El-Didy, S.M2, Eizeldin, M.A3, and Helmi, A.M4 ﻣﻠﺨﺺ ﻋﺮﺑﻲ ﺗﻢ إﻋﺪاد اﻟﻌﺪﯾﺪ ﻣﻦ اﻟﺪراﺳﺎت - ﻓﻲ ﺑﺪاﯾﺔ اﻟﻘﺮن اﻟﻌﺸﺮﯾﻦ - ﻟﺪراﺳﺔ ﺗﻮﺻﯿﻞ ﻣﯿﺎه اﻟﺒﺤﺮ اﻟﻤﺘﻮﺳﻂ ﻣﻦ ﺧﻼل ﻗﻨﺎة ﺗﻮﺻﯿﻞ ﻟﻤﻨﺨﻔﺾ اﻟﻘﻄﺎرة ﺑﮭﺪف ﺗﻮﻟﯿﺪ اﻟﻄﺎﻗﺔ اﻟﻜﮭﺮﺑﺎﺋﯿﺔ وذﻟﻚ ﺑﺈﺳﺘﻐﻼل ﻓﺮق اﻟﻤﻨﺎﺳﯿﺐ ﺑﯿﻦ اﻟﻤﻨﺨﻔﺾ واﻟﺒﺤﺮ اﻟﻤﺘﻮﺳﻂ ، وﺗﮭﺪف اﻟﺪراﺳﺔ اﻟﺤﺎﻟﯿﺔ إﻟﻰ :-أ) إﻧﺸﺎء ﻣﻨﻈﻮﻣﺔ ﻣﻌﻠﻮﻣﺎت ھﯿﺪروﻟﻮﺟﯿﺔ ﻟﻠﻤﻨﺨﻔﺾ ب) ﺣﺴﺎب ﻣﻌﺪﻻت اﻟﺒﺨﺮ اﻟﻤﺘﻮﻗﻊ ﻣﻦ اﻟﻤﯿﺎه اﻟﻤﺎﻟﺤﺔ اﻟﻤﺠﻤﻌﺔ ﻓﻲ ﺑﺤﯿﺮة اﻟﻤﻨﺨﻔﺾ. وﻗﺪ ﺗﻢ إﻋﺪاد ﻣﻨﮭﺞ اﻟﺪراﺳﺔ ﺑﺎﺳﺘﺨﺪام اﻟﺒﺮاﻣﺞ اﻟﺤﺪﯾﺜﺔ اﻟﺘﻲ ﻟﻢ ﺗﻜﻦ ﻣﺘﺎﺣﺔ ﻟﻠﺪراﺳﺎت اﻟﺴﺎﺑﻘﺔ ﻟﻠﻤﺸﺮوع ﺣﯿﻨﮭﺎ، وھﺬه اﻟﺒﺮاﻣﺞ ﻣﺜﻞ اﻟﻨﻤﺎذج اﻟﻌﺪدﯾﺔ اﻟﻔﻌﺎﻟﺔ، ﻧﻈﺎم اﻟﻤﻌﻠﻮﻣﺎت اﻟﻌﺪدﯾﺔ ( GIS) ، وﻧﻤﺎذج اﻹرﺗﻔﺎﻋﺎت اﻟﺮﻗﻤﯿﺔ (DEM). -
Taconic Physiography
Bulletin No. 272 ' Series B, Descriptive Geology, 74 DEPARTMENT OF THE INTERIOR . UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR 4 t TACONIC PHYSIOGRAPHY BY T. NELSON DALE WASHINGTON GOVERNMENT PRINTING OFFICE 1905 CONTENTS. Page. Letter of transinittal......................................._......--..... 7 Introduction..........I..................................................... 9 Literature...........:.......................... ........................... 9 Land form __._..___.._.___________..___._____......__..__...._..._--..-..... 18 Green Mountain Range ..................... .......................... 18 Taconic Range .............................'............:.............. 19 Transverse valleys._-_-_.-..._.-......-....___-..-___-_....--_.-.._-- 19 Longitudinal valleys ............................................. ^...... 20 Bensselaer Plateau .................................................... 20 Hudson-Champlain valley................ ..-,..-.-.--.----.-..-...... 21 The Taconic landscape..................................................... 21 The lakes............................................................ 22 Topographic types .............,.....:..............'.................... 23 Plateau type ...--....---....-.-.-.-.--....-...... --.---.-.-..-.--... 23 Taconic type ...-..........-........-----............--......----.-.-- 28 Hudson-Champlain type ......................"...............--....... 23 Rock material..........................'.......'..---..-.....-...-.--.-.-. 23 Harder rocks ....---...............-.-.....-.-...--.-......... -
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. -
South Carolina Landform Regions (And Facts About Landforms) Earth Where Is South Carolina? North America United States of America SC
SCSouth Carolina Landform Regions (and facts about Landforms) Earth Where is South Carolina? North America United States of America SC Here we are! South Carolina borders the Atlantic Ocean. SC South Carolina Landform Regions Map Our state is divided into regions, starting at the mountains and going down to the coast. Can you name these? Blue Ridge Mountains Landform Regions SC The Blue Ridge Mountain Region is only 2% of the South Carolina land mass. Facts About the Blue Ridge Mountains . ◼ It is the smallest of the landform regions ◼ It includes the state’s highest point: Sassafras Mountain. ◼ The Blue Ridge Mountains are part of the Appalachian Mountain Range Facts About the Blue Ridge Mountains . ◼ The Blue Ridge Region is mountainous and has many hardwood forests, streams, and waterfalls. ◼ Many rivers flow out of the Blue Ridge. Blue Ridge Mountains, SC Greenville Spartanburg Union Greenwood Rock Hill Abbeville Piedmont Landform Regions SC If you could see the Piedmont Region from space and without the foliage, you would notice it is sort of a huge plateau. Facts About the Piedmont Region . ◼ The Piedmont is the largest region of South Carolina. ◼ The Piedmont is often called The Upstate. Facts About the Piedmont Region . ◼ It is the foothills of the mountains and includes rolling hills and many valleys. ◼ Piedmont means “foot of the mountains” ◼ Waterfalls and swift flowing rivers provided the water power for early mills and the textile industry. Facts About the Piedmont Region . ◼ The monadnocks are located in the Piedmont. ◼ Monadnocks – an isolated or single hill made of very hard rock. -
ED052034.Pdf
DOCUMENT RESUME ED 052 034 SE 011 371 AUTHOR Reiners, William A.; Smallwood, Frank TITLE Undergraduate Education in Environmental Studies, A Conference Report. INSTITUTION Dartmouth Coll., Hanover, N.H. PUB DATE Apr 70 NOTE 100p. AVAILABLE FROM Public Affiars Center E Dartmouth Bicentennial Year Committee, Dartmouth College, Hanover, New Hampshire ($2.50) EDRS PRICE EDRS price MF-$0.65 HC-$3.29 DESCRIPTORS College Programs, Conference Reports, Curriculum, *Curriculum Development, *Environment, *Environmental Education, Program Descriptions, *Program Development, Programs, *Undergraduate Study ABSTRACT The nine papers included in this volume were presented during the "Working Conference on Undergraduate Education in Environmental Studies" at Dartmouth College. The rationale and strategy for environmental studies at Dartmouth College are considered in part one. Details of the proposed programs at both Dartmouth College and Williams College are reviewed in the concluding section. The main body of the volume consists of four working papers, each designed to provide a specific in-depth analysis of a key issue related to environmental education: Bioeconomics--The Science of Survival: A Proposed Philosophy for the Program; Basic approaches to the Organization of a Curriculum; Environmental Centers in a Crowded Landscape: Policies and Pitfalls in Organizing a Program; and A Case Study of New England: Examples of Public and Private Support for Environmental Education. Two additional conference papers are included: Man and Nature on Collision Course; and Environmental Dialogue: The New Education. (PR) U.S. DEPARTMENT OF HEALTH. EDUCATION & WELFARE OFFICE DF EDUCATION THIS DOCUMENT HAS BEENREPRO- OUCED EXACTLY AS RECEIVED FROM THE PERSON OR ORGANIZATIONORIG- INATING IT. POINTS OF VIEW OR OPIN- IONS STATED DO NOT NECESSARILY REPRESENT OFFICIAL OFFICE OF EDU- CATION POSITION OR POLICY A CONFERENCE REPORT Undergraduate Education in Environmental Studies EDITED BY WILLIAM A. -
The Levee Was Sparsely Vegetated by Pioneering Species Like Blazing Star, Russian Thistle, Sweet White Clover, and Seedlings Of
Upper Carson River Watershed Stream Corridor Assessment The levee was sparsely vegetated by pioneering species like blazing star, Russian thistle, sweet white clover, and seedlings of mountain big sagebrush and rubber rabbitbrush. Large, mature black cottonwoods occupied the stream terrace at the upper cross section location on the right side, providing picnic and camp sites for area recreationists. Past beaver activity (+/-10 years) was indicated by a 12 inch diameter cottonwood stump. The herabaceous understory was sparse to absent. The topographic depression located between the levee and the highway was developing into an emergent wetland community dominated by cattail. At the higher end of this depression (where it was drier), a large stand of bull thistle was present. Coyote willows also occupied the drying end of this area. A woody regeneration transect was established adjacent to the right side of the river on an elevated terrace. Mature black cottonwood provided an almost continuous canopy cover. The age class distribution of the woody species showed a ratio of approximately 2.7:1 sprout and saplings to mature, decadent, and dead black cottonwood, woods rose, mountain alder and willow species. Data developed as part of the present study (Table 4.10) indicate that the area is dominated by early and mid successional status ratings. Vegetation in the area is adjusting to past disturbances (recreation) and current fluvial processes. Table 4.10. Reach EF7 successional status data. Successional Percent Status Occurrence Early 43.4 Mid 32.9 High 23.8 A management recommendation would be to remove the existing bull thistle stand and monitor to prevent its reestablishment. -
Geomorphometry of Cerro Sillajhuay (Andes, Chile/Bolivia): Comparison of Digital Elevation Models (Dems) from ASTER Remote Sensing Data and Contour Maps
Geomorphometry of Cerro Sillajhuay (Andes, Chile/Bolivia): Comparison of Digital Elevation Models (DEMs) from ASTER Remote Sensing Data and Contour Maps Ulrich Kamp Department of Geography and Environmental Science Program, DePaul University 990 W Fullerton Ave, Chicago, IL 60614-2458, U.S.A. E-mail: [email protected] Tobias Bolch Department of Geography, Humboldt University Berlin Rudower Chausse 16, Unter den Linden 6, 10099 Berlin, Germany E-mail: [email protected] Jeffrey Olsenholler Department of Geography and Geology, University of Nebraska - Omaha 6001 Dodge Street, Omaha, NE 68182-0199, U.S.A. [email protected] Abstract Digital elevation models (DEMs) are increasingly used for visual and mathematical analysis of topography, landscapes and landforms, as well as modeling of surface processes. To accomplish this, the DEM must represent the terrain as accurately as possible, since the accuracy of the DEM determines the reliability of the geomorphometric analysis. For Cerro Sillajhuay in the Andes of Chile/Bolivia two DEMs are compared: one derived from contour maps, the other from a satellite stereo-pair from the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER). As both DEM procedures produce estimates of elevation, quantative analysis of each DEM was limited. The original ASTER DEM has a horizontal resolution of 30 m and was generated using tie points (TPs) and ground control points (GCPs). It was then resampled to 15 m resolution, the resolution of the VNIR bands. Five parameters were calculated for geomorphometric interpretation: elevation, slope angle, slope aspect, vertical curvature, and tangential curvature. Other calculations include flow lines and solar radiation. -
Street Names - in Alphabetical Order
Street Names - In Alphabetical Order District / MC-ID NO. Street Name Location County Area Aalto Place Sumter - Unit 692 (Villa San Antonio) 1 Sumter County Abaco Path Sumter - Unit 197 9 Sumter County Abana Path Sumter - Unit 206 9 Sumter County Abasco Court Sumter - Unit 821 (Mangrove Villas) 8 Sumter County Abbeville Loop Sumter - Unit 80 5 Sumter County Abbey Way Sumter - Unit 164 8 Sumter County Abdella Way Sumter - Unit 180 9 Sumter County Abdella Way Sumter - Unit 181 9 Sumter County Abel Place Sumter - Unit 195 10 Sumter County Aber Lane Sumter - Unit 967 (Ventura Villas) 10 Sumter County SE 84TH Abercorn Court Marion - Unit 45 4 Marion County Abercrombie Way Sumter - Unit 98 5 Sumter County Aberdeen Run Sumter - Unit 139 7 Sumter County Abernethy Place Sumter - Unit 99 5 Sumter County Abner Street Sumter - Unit 130 6 Sumter County Abney Avenue VOF - Unit 8 12 Sumter County Abordale Lane Sumter - Unit 158 8 Sumter County Acorn Court Sumter - Unit 146 7 Sumter County Acosta Court Sumter - Unit 601 (Villa De Leon) 2 Sumter County Adair Lane Sumter - Unit 818 (Jacaranda Villas) 8 Sumter County Adams Lane Sumter - Unit 105 6 Sumter County Adamsville Avenue VOF - Unit 13 12 Sumter County Addison Avenue Sumter - Unit 37 3 Sumter County Adeline Way Sumter - Unit 713 (Hillcrest Villas) 7 Sumter County Adelphi Avenue Sumter - Unit 151 8 Sumter County Adler Court Sumter - Unit 134 7 Sumter County Adriana Way Sumter - Unit 711 (Adriana Villas) 7 Sumter County Adrienne Way Sumter - Unit 176 9 Sumter County Adrienne Way Sumter - Unit 949 (Megan -
Bag of Geomorphological Words: a Framework for Integrating Terrain
International Journal of Geo-Information Article Bag of Geomorphological Words: A Framework for Integrating Terrain Features and Semantics to Support Landform Object Recognition from High-Resolution Digital Elevation Models Xiran Zhou 1,2 , Xiao Xie 3,* , Yong Xue 1,2, Bing Xue 3 , Kai Qin 1,2 and Weijiang Dai 4 1 School of Environment and Spatial Informatics, China University of Mining and Technology, Xuzhou 221116, China; [email protected] (X.Z.); [email protected] (Y.X.); [email protected] (K.Q.) 2 Artificial Intelligence Research Institute, China University of Mining and Technology, Xuzhou 221116, China 3 Key Laboratory for Environment Computation & Sustainability of Liaoning Province, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; [email protected] 4 Nuclear Industry Huzhou Engineering Investigation Institute, Huzhou 313000, China; [email protected] * Correspondence: [email protected] Received: 7 July 2020; Accepted: 18 October 2020; Published: 23 October 2020 Abstract: High-resolution digital elevation models (DEMs) and its derivatives (e.g., curvature, slope, aspect) offer a great possibility of representing the details of Earth’s surface in three-dimensional space. Previous research investigations concerning geomorphological variables and region-level features alone cannot precisely characterize the main structure of landforms. However, these geomorphological variables are not sufficient to represent a complex landform object’s whole structure from a high-resolution DEM. Moreover, the amount of the DEM dataset is limited, including the landform object. Considering the challenges above, this paper reports an integrated model called the bag of geomorphological words (BoGW), enabling automatic landform recognition via integrating point and linear geomorphological variables, region-based features (e.g., shape, texture), and high-level landform descriptions.