Visual Exposure of Rock Outcrops in the Context of a Forest Disease
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Révision Taxinomique Et Nomenclaturale Des Rhopalocera Et Des Zygaenidae De France Métropolitaine
Direction de la Recherche, de l’Expertise et de la Valorisation Direction Déléguée au Développement Durable, à la Conservation de la Nature et à l’Expertise Service du Patrimoine Naturel Dupont P, Luquet G. Chr., Demerges D., Drouet E. Révision taxinomique et nomenclaturale des Rhopalocera et des Zygaenidae de France métropolitaine. Conséquences sur l’acquisition et la gestion des données d’inventaire. Rapport SPN 2013 - 19 (Septembre 2013) Dupont (Pascal), Demerges (David), Drouet (Eric) et Luquet (Gérard Chr.). 2013. Révision systématique, taxinomique et nomenclaturale des Rhopalocera et des Zygaenidae de France métropolitaine. Conséquences sur l’acquisition et la gestion des données d’inventaire. Rapport MMNHN-SPN 2013 - 19, 201 p. Résumé : Les études de phylogénie moléculaire sur les Lépidoptères Rhopalocères et Zygènes sont de plus en plus nombreuses ces dernières années modifiant la systématique et la taxinomie de ces deux groupes. Une mise à jour complète est réalisée dans ce travail. Un cadre décisionnel a été élaboré pour les niveaux spécifiques et infra-spécifique avec une approche intégrative de la taxinomie. Ce cadre intégre notamment un aspect biogéographique en tenant compte des zones-refuges potentielles pour les espèces au cours du dernier maximum glaciaire. Cette démarche permet d’avoir une approche homogène pour le classement des taxa aux niveaux spécifiques et infra-spécifiques. Les conséquences pour l’acquisition des données dans le cadre d’un inventaire national sont développées. Summary : Studies on molecular phylogenies of Butterflies and Burnets have been increasingly frequent in the recent years, changing the systematics and taxonomy of these two groups. A full update has been performed in this work. -
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. -
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. -
LIME: Software for 3-D Visualization, Interpretation, and Communication of Virtual Geoscience Models Simon J
LIME: Software for 3-D visualization, interpretation, and communication of virtual geoscience models Simon J. Buckley, Kari Ringdal, Nicole Naumann, Benjamin Dolva, Tobias H. Kurz, John A. Howell, Thomas Dewez To cite this version: Simon J. Buckley, Kari Ringdal, Nicole Naumann, Benjamin Dolva, Tobias H. Kurz, et al.. LIME: Software for 3-D visualization, interpretation, and communication of virtual geoscience models. Geo- sphere, Geological Society of America, 2019, 15, pp.222-235. 10.1130/GES02002.1. hal-02380693 HAL Id: hal-02380693 https://hal.archives-ouvertes.fr/hal-02380693 Submitted on 28 Nov 2019 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. Software Contribution GEOSPHERE LIME: Software for 3-D visualization, interpretation, and communication of virtual geoscience models GEOSPHERE, v. 15, no. 1 Simon J. Buckley1,2, Kari Ringdal1, Nicole Naumann1, Benjamin Dolva1, Tobias H. Kurz1, John A. Howell3, and Thomas J.B. Dewez4 1NORCE Norwegian Research Centre AS, P.O. Box 22, N-5838 Bergen, Norway https://doi.org/10.1130/GES02002.1 2Department of Earth Science, University of Bergen, P.O. Box 7803, N-5020 Bergen, Norway 3Department of Geology and Petroleum Geology, University of Aberdeen, Aberdeen AB24 3UE, UK 9 figures 4BRGM–French Geological Survey, 45060 Orléans, France CORRESPONDENCE: [email protected] ABSTRACT science, volcanology, natural hazards, hydrology, energy, infrastructure, and CITATION: Buckley, S.J., Ringdal, K., Naumann, N., Dolva, B., Kurz, T.H., Howell, J.A., and Dewez, mining). -
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 -
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 -
Petroleum Geological Analysis Based on Remote Sensing and Laser Scanning in Karamay Formation of Junggar Basin, China
E3S Web of Conferences 206, 01023 (2020) https://doi.org/10.1051/e3sconf/202020601023 ICGEC 2020 Petroleum Geological Analysis Based on Remote Sensing and laser scanning in Karamay Formation of Junggar Basin, China Qihong Zeng1, Youyan Zhang 1, Linghua Kong 2, Yong Ye 1, Yan Hu 1, Wenzhi Wang 1 and Yuanyuan Chen3* 1Research Institute of Petroleum Exploration&Development, Petro China, Beijing,100083, China 2Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang, 834000, China 3 University of Science and Technology LiaoNing, Anshan,114051, China Abstract. This paper uses high-precision remote sensing and laser scanning to study petroleum geological analysis methods. The research area is Karamay Formation in Junggar Basin, China. Firstly, the outcrop lithologies are identified according to our clastic rock lithology identification pattern based on laser intensity, and the regional lithologies are identified based on high-precision remote sensing images. Furthermore, we analyze the horizontal and vertical distribution characteristics of the sandbodies. At last, we analyze the area sandbody connectivity and sandbody structure characteristics. These data can provide basic information for the analysis of underground reservoirs in Karamay Formation. 1 Introduction Digital outcrop is an effective method to realize the 2 Geological background of the study research of underground reservoir analogues. The digital area outcrop based on remote sensing and ground laser scanning can study the outcrop reservoir structure The Karamay Formation and Baikouquan Formation of intuitively, quantitatively and precisely . the Triassic strata in the northwestern margin of the Lidar can quickly and accurately obtain the 3D Junggar Basin are the main productive layers, mainly information of the measured object, and establish a with coarse clastic deposits. -
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. -
Quantitative Characterization of a Naturally Fractured Reservoir Analog
Research Paper GEOSPHERE Quantitative characterization of a naturally fractured reservoir GEOSPHERE; v. 14, no. 2 analog using a hybrid lidar-gigapixel imaging approach doi:10.1130/GES01449.1 Kivanc Biber1,2, Shuhab D. Khan1, Thomas D. Seers3, Sergio Sarmiento4, and M.R. Lakshmikantha4 1 14 figures; 7 tables Department of Earth and Atmospheric Sciences, University of Houston, 4800 Calhoun Road, Houston, Texas 77004, USA 2Statoil North America, 2107 CityWest Boulevard, Houston, Texas 77042, USA 3Department of Petroleum Engineering, Texas A&M University at Qatar Engineering Building, Education City, Doha, Qatar 23874 CORRESPONDENCE: kbiber@ uh .edu 4Repsol USA, Technology Hub, 2455 Technology Forest Boulevard, The Woodlands, Texas 77381, USA CITATION: Biber, K., Khan, S.D., Seers, T.D., Sarmiento, S., and Lakshmikantha, M.R., 2018, Quantitative characterization of a naturally fractured ABSTRACT 1. INTRODUCTION reservoir analog using a hybrid lidar-gigapixel imag- ing approach: Geosphere, v. 14, no. 2, p. 710–730, The inability to accurately resolve subseismic-scale structural discontinui- Understanding the orientation distribution and spatial configuration of doi:10.1130/GES01449.1. ties such as natural fractures represents a significant source of uncertainty natural fractures is important because these structural discontinuities signifi- for subsurface modeling practices. Fracture statistics collected from outcrop cantly influence the behavior of many oil and gas reservoirs. As such, they Science Editor: Raymond M. Russo Associate Editor: Francesco Mazzarini analogs are commonly used to fill the knowledge gap to reduce the uncer- impact fluid flow (e.g., Wilson et al., 2011b) and geomechanical state of the tainty related to fracture-induced permeability anisotropy. The conventional reservoirs (e.g., Heffer, 2012; Couples, 2013). -
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. -
Low-Cost Prototype to Automate the 3D Digitization of Pieces: an Application Example and Comparison
sensors Article Low-Cost Prototype to Automate the 3D Digitization of Pieces: An Application Example and Comparison Ramón González-Merino 1, Elena Sánchez-López 2,*, Pablo E. Romero 3 , Jesús Rodero 1 and Rafael E. Hidalgo-Fernández 2 1 Technology Centre of Metal-Mechanical and Transport, Department of Visual Computing, 23700 Linares, Spain; [email protected] (R.G.-M.); [email protected] (J.R.) 2 Department of Graphic and Geomatic Engineering, Campus of Rabanales, University of Córdoba, 14014 Córdoba, Spain; [email protected] 3 Department of Mechanical Engineering, Campus of Rabanales, University of Córdoba, 14014 Córdoba, Spain; [email protected] * Correspondence: [email protected] Abstract: This work is aimed at describing the design of a mechanical and programmable 3D capturing system to be used by either 3D scanner or DSLR camera through photogrammetry. Both methods are widely used in diverse areas, from engineering, architecture or archaeology, up to the field of medicine; but they also entail certain disadvantages, such as the high costs of certain equipment, such as scanners with some precision, and the need to resort to specialized operatives, among others. The purpose of this design is to create a robust, precise and cost-effective system that improves the limitations of the present equipment on the market, such as robotic arms or rotary tables. For this reason, a preliminary study has been conducted to analyse the needs of improvement, Citation: González-Merino, R.; later, we have focused on the 3D design and prototyping. For its construction, there have been used Sánchez-López, E.; Romero, P.E.; the FDM additive technology and structural components that are easy to find in the market. -
The Fluctuating Asymmetry of the Butterfly Wing Pattern Does Not Change Along an Industrial Pollution Gradient
S S symmetry Article The Fluctuating Asymmetry of the Butterfly Wing Pattern Does Not Change along an Industrial Pollution Gradient Vitali Zverev and Mikhail V. Kozlov * Department of Biology, University of Turku, 20014 Turku, Finland; vitzve@utu.fi * Correspondence: mikoz@utu.fi Abstract: The rapid and selective responses to changes in habitat structure and climate have made butterflies valuable environmental indicators. In this study, we asked whether the decline in butterfly populations near the copper-nickel smelter in Monchegorsk in northwestern Russia is accompanied by phenotypic stress responses to toxic pollutants, expressed as a decrease in body size and an increase in fluctuating asymmetry. We measured the concentrations of nickel and copper, forewing length, and fluctuating asymmetry in two elements of wing patterns in Boloria euphrosyne, Plebejus idas, and Agriades optilete collected 1–65 km from Monchegorsk. Body metal concentrations increased toward the smelter, confirming the local origin of the collected butterflies. The wings of butterflies from the most polluted sites were 5–8% shorter than those in unpolluted localities, suggesting adverse effects of pollution on butterfly fitness due to larval feeding on contaminated plants. However, fluctuating asymmetry averaged across two hindwing spots did not change systematically with pollution, thereby questioning the use of fluctuating asymmetry as an indicator of habitat quality in butterfly conservation projects. Keywords: copper-nickel smelter; fluctuating asymmetry; Kola Peninsula; Lepidoptera; phenotypic Citation: Zverev, V.; Kozlov, M.V. stress responses; wing length The Fluctuating Asymmetry of the Butterfly Wing Pattern Does Not Change along an Industrial Pollution Gradient. Symmetry 2021, 13, 626. https://doi.org/10.3390/sym13040626 1.