Description of the Igneous Formations
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Hadrian and the Greek East
HADRIAN AND THE GREEK EAST: IMPERIAL POLICY AND COMMUNICATION DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of the Ohio State University By Demetrios Kritsotakis, B.A, M.A. * * * * * The Ohio State University 2008 Dissertation Committee: Approved by Professor Fritz Graf, Adviser Professor Tom Hawkins ____________________________ Professor Anthony Kaldellis Adviser Greek and Latin Graduate Program Copyright by Demetrios Kritsotakis 2008 ABSTRACT The Roman Emperor Hadrian pursued a policy of unification of the vast Empire. After his accession, he abandoned the expansionist policy of his predecessor Trajan and focused on securing the frontiers of the empire and on maintaining its stability. Of the utmost importance was the further integration and participation in his program of the peoples of the Greek East, especially of the Greek mainland and Asia Minor. Hadrian now invited them to become active members of the empire. By his lengthy travels and benefactions to the people of the region and by the creation of the Panhellenion, Hadrian attempted to create a second center of the Empire. Rome, in the West, was the first center; now a second one, in the East, would draw together the Greek people on both sides of the Aegean Sea. Thus he could accelerate the unification of the empire by focusing on its two most important elements, Romans and Greeks. Hadrian channeled his intentions in a number of ways, including the use of specific iconographical types on the coinage of his reign and religious language and themes in his interactions with the Greeks. In both cases it becomes evident that the Greeks not only understood his messages, but they also reacted in a positive way. -
Bedrock Geology Glossary from the Roadside Geology of Minnesota, Richard W
Minnesota Bedrock Geology Glossary From the Roadside Geology of Minnesota, Richard W. Ojakangas Sedimentary Rock Types in Minnesota Rocks that formed from the consolidation of loose sediment Conglomerate: A coarse-grained sedimentary rock composed of pebbles, cobbles, or boul- ders set in a fine-grained matrix of silt and sand. Dolostone: A sedimentary rock composed of the mineral dolomite, a calcium magnesium car- bonate. Graywacke: A sedimentary rock made primarily of mud and sand, often deposited by turbidi- ty currents. Iron-formation: A thinly bedded sedimentary rock containing more than 15 percent iron. Limestone: A sedimentary rock composed of calcium carbonate. Mudstone: A sedimentary rock composed of mud. Sandstone: A sedimentary rock made primarily of sand. Shale: A deposit of clay, silt, or mud solidified into more or less a solid rock. Siltstone: A sedimentary rock made primarily of sand. Igneous and Volcanic Rock Types in Minnesota Rocks that solidified from cooling of molten magma Basalt: A black or dark grey volcanic rock that consists mainly of microscopic crystals of pla- gioclase feldspar, pyroxene, and perhaps olivine. Diorite: A plutonic igneous rock intermediate in composition between granite and gabbro. Gabbro: A dark igneous rock consisting mainly of plagioclase and pyroxene in crystals large enough to see with a simple magnifier. Gabbro has the same composition as basalt but contains much larger mineral grains because it cooled at depth over a longer period of time. Granite: An igneous rock composed mostly of orthoclase feldspar and quartz in grains large enough to see without using a magnifier. Most granites also contain mica and amphibole Rhyolite: A felsic (light-colored) volcanic rock, the extrusive equivalent of granite. -
Fact Sheet 5 Principles of Stone Extraction
QuarryScapes guide to ancient stone quarries Fact Sheet 5 Fact Sheet 5 Principles of stone extraction In all stone quarry situations the extraction phase rich) ones. Partly because they in general display is based on one or combinations of three the most brittle behaviour, but also because it is a fundamental principles: well documented fact (and experience among quarrymen) that siliceous rocks (granite in 1. Levering; expanding open fractures by particular) have well defined preferred splitting inserting levers, crowbars or stones 2. Splitting; creating fractures, preferable directions defined by microfractures in quartz. planar, by strokes (i.e. sledge hammer), Splitting by heating is caused by a combination of wedging; heating or blasting with thermal expansion properties and brittle explosives behaviour. It works best on quartz-rich rocks due 3. Channelling (carving); making channels in to the well known but poorly understood change the rock by carving with hammer and of mechanical properties of quartz when heated. chisel, pickaxe or stone tools, heating with fire, sawing or drilling Channelling is the third fundamental principle. Channels in the rock are made by removing the Levering may be described as the “simplest” way rock mass by chiselling, picking, sawing or of extraction, involving the expansion of natural heating. In most soft stone quarries from the cracks or other planes of weakness (such as Bronze Age onwards, channelling is the most bedding planes) using various tools. important extraction method. In most cases, channelling is combined with other methods. For Splitting may be defined as the act of generating instance, channels are made perpendicular to the new fractures for extracting rock. -
Jackson Hole Vacation Planner Vacation Hole Jackson Guide’S Guide Guide’S Globe Addition Guide Guide’S Guide’S Guide Guide’S
TTypefypefaceace “Skirt” “Skirt” lightlight w weighteight GlobeGlobe Addition Addition Book Spine Book Spine Guide’s Guide’s Guide’s Guide Guide’s Guide Guide Guide Guide’sGuide’s GuideGuide™™ Jackson Hole Vacation Planner Jackson Hole Vacation2016 Planner EDITION 2016 EDITION Typeface “Skirt” light weight Globe Addition Book Spine Guide’s Guide’s Guide Guide Guide’s Guide™ Jackson Hole Vacation Planner 2016 EDITION Welcome! Jackson Hole was recognized as an outdoor paradise by the native Americans that first explored the area thousands of years before the first white mountain men stumbled upon the valley. These lucky first inhabitants were here to hunt, fish, trap and explore the rugged terrain and enjoy the abundance of natural resources. As the early white explorers trapped, hunted and mapped the region, it didn’t take long before word got out and tourism in Jackson Hole was born. Urbanites from the eastern cities made their way to this remote corner of northwest Wyoming to enjoy the impressive vistas and bounty of fish and game in the name of sport. These travelers needed guides to the area and the first trappers stepped in to fill the niche. Over time dude ranches were built to house and feed the guests in addition to roads, trails and passes through the mountains. With time newer outdoor pursuits were being realized including rafting, climbing and skiing. Today Jackson Hole is home to two of the world’s most famous national parks, world class skiing, hiking, fishing, climbing, horseback riding, snowmobiling and wildlife viewing all in a place that has been carefully protected allowing guests today to enjoy the abundance experienced by the earliest explorers. -
Chapter 2 Alaska’S Igneous Rocks
Chapter 2 Alaska’s Igneous Rocks Resources • Alaska Department of Natural Resources, 2010, Division of Geological and Geophysical Surveys, Alaska Geologic Materials Center website, accessed May 27, 2010, at http://www.dggs.dnr.state.ak.us/?link=gmc_overview&menu_link=gmc. • Alaska Resource Education: Alaska Resource Education website, accessed February 22, 2011, at http://www.akresource.org/. • Barton, K.E., Howell, D.G., and Vigil, J.F., 2003, The North America tapestry of time and terrain: U.S. Geological Survey Geologic Investigations Series I-2781, 1 sheet. (Also available at http://pubs.usgs.gov/imap/i2781/.) • Danaher, Hugh, 2006, Mineral identification project website, accessed May 27, 2010, at http://www.fremontica.com/minerals/. • Digital Library for Earth System Education, [n.d.], Find a resource—Bowens reaction series: Digital Library for Earth System Education website, accessed June 10, 2010, at http://www.dlese.org/library/query.do?q=Bowens%20reaction%20series&s=0. • Edwards, L.E., and Pojeta, J., Jr., 1997, Fossils, rocks, and time: U.S. Geological Survey website. (Available at http://pubs.usgs.gov/gip/fossils/contents.html.) • Garden Buildings Direct, 2010, Rocks and minerals: Garden Buildings Direct website, accessed June 4, 2010, at http://www.gardenbuildingsdirect.co.uk/Article/rocks-and- minerals. • Illinois State Museum, 2003, Geology online–GeoGallery: Illinois State Museum Society database, accessed May 27, 2010 at http://geologyonline.museum.state.il.us/geogallery/. • Knecht, Elizebeth, designer, Pearson, R.W., and Hermans, Majorie, eds., 1998, Alaska in maps—A thematic atlas: Alaska Geographic Society, 100 p. Lillie, R.J., 2005, Parks and plates—The geology of our National parks, monuments, and seashores: New York, W.W. -
Economic Geology Report ER79-4: Porphyritic Intrusions and Related
MANITOBA CANADA DEPARTMENT OF ENERGY AND MINES MANITOBA MINERAL RESOURCES DIVISION ECONOMIC GEOLOGY REPORT ER79-4 PORPHYRITIC INTRUSIONS AND RELATED MINERALIZATION IN THE FLIN FLON VOLCANIC BELT by D.A. BALDWIN 1980 Funding for this project was provided under the cost-shared Canada-Manitoba Non-renewable Resources Evaluation Program by the Canada Department of Energy, Mines and Resources and the Manitoba Department of Mines, Resources and Environmental Management. MANITOBA DEPARTMENT OF ENERGY AND MINES HON. DONALD W. CRAIK PAUL E. JARVIS Minister Deputy Minister MINERAL RESOURCES DIVISION IAN HAUGH Executive Director ECONOMIC GEOLOGY REPORT ER79-4 PORPHYRITIC INTRUSIONS AND RELATED MINERALIZATION IN THE FLIN FLON VOLCANIC BELT by D.A. BALDWIN 1980 LEGEND I Cliff Lake Stock 5 Elbow Lake Stock 2 Whitefish Lake Porphyry 6 Fourmile Island Intrusion 3 Alberts Lake Intrusion 7 Chisel Lake Intrusion 4 Nisto Lake Intrusion 8 Wekusko Lake Intrusion ,~ -./ - -, I \." ~herridon '" , ;. <,.... ,1 if 55°00' 55°00' c, t,:) ,J -3 , I"" . c;? '" 1[' . ::t} \'''If!? ~,/J~ /j' ., ~), F lin.~ i;\))F ' I,".!0l~' ,d ' ;)/", ' ~.;'. l ;' ~" ,r~n ;t j; (I:/,1 ,r Lake ' \\ ;\~ ' ~i'/ 'lUi':;- -'i' //{ ,'/ , ,\" ,,/,1,1 pI , .h .(,1;' '\:. (IiI' ' .. '~'4_hl i / 'Y{j,'{:" 5 2.5 a 10 15 KILOMETRES J!) "'.t3 f3,F-"\ ---- :i~ f)J~c~. V 99°30' ">/)AfhapaplJskoj¥ !ZJ Porphyritic Intrusive Rocks 54°30' ! ,1 Lake .; ... 100°30' D Felsic Volcanic Rocks FIGURE 1: Distribution of porphyritic intrusive and felsic volcanic rocks in the Flin Flon volcanic belt, TABLE OF -
Petrographic Study of a Quartz Diorite Stock Near Superior, Pinal County, Arizona
Petrographic study of a quartz diorite stock near Superior, Pinal County, Arizona Item Type text; Thesis-Reproduction (electronic); maps Authors Puckett, James Carl, 1940- 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 23/09/2021 23:40:37 Link to Item http://hdl.handle.net/10150/554062 PETROGRAPHIC STUDY OF A QUARTZ DIORITE STOCK NEAR SUPERIOR, PINAL COUNTY, ARIZONA by James Carl Puckett, Jr. A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOLOGY In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 1 9 7 0 STATEMENT BY AUTHOR This thesis has been submitted in partial fulfillment of re quirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable without special permission, provided that accurate acknowledgment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major department or the Dean of the Graduate College when in his judg ment the proposed use of the material is in the interests of scholar ship. In all other instances, however, permission must be obtained from the author. -
Smithsonian Miscellaneous Collections
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 103. NUMBER 5 NEW UPPER CAMBRIAN TRILOBITES (With 21 Plates) BY CHARLES E. RESSER Curator, Division of Invertebrate Paleontology and Paleobotany U. S. National Museum (Publication 3693) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION OCTOBER 21, 1942 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 103. NUMBER 5 NEW UPPER CAMBRIAN TRILOBITES (With 21 Plates) BY CHARLES E. RESSER Curator, Division of Invertebrate Paleontology and Paleobotany U. S. National Museum (Publication 3693) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION OCTOBER 21, 1942 BALTIMORE, MD., U. S. A. CONTENTS PAGE Introduction i Description of genera and species 2 Komaspidae Kobayashi 2 Chariocephalus Hall 4 Irvingella Ulrich and Resser 13 Parairvingella Kobayashi 25 Drumaspis, new genus 28 Unclassified genera 35 Cheilocephalns Berkey 35 Cholopilus Raymond 36 Caiyptonima, new genus 37 Illaenurus Hall 38 Platycolpus Raymond 40 Enontioura, new genus 42 Macclloura Resser 43 Arapahoia Miller 43 Plethomctopus Ulrich 47 Kingstonia VValcott 47 Byniunia Walcott 52 BynumicUa, new genus 57 Bynumina, new genus 58 Stenopilns Raymond 59 Blountia Walcott 60 Blountiella Resser 61 Ellipsocephaloides Kobayashi 62 MaryviUia Walcott 67 Meteoraspis Resser 72 Coosia Walcott 73 Coosella Lochman 75 Ptcroccphalina Resser 76 Burnetidae, new family 79 Burnetia Walcott 80 Iddingsia Walcott 85 Berkeia Resser 90 Unclassified genera 94 Elvinia Walcott 94 Taenicephalus Ulrich and Resser 99 Talbotina Lochman 107 Explanation of plates 109 Index 131 iii NEW UPPER CAMBRIAN TRILOBITES By CHARLES E. RESSER Curator, Division of Invertebrate Paleontology and Paleobotany, U. S. National Museum (With 21 Plates) INTRODUCTION Soon after 1878 when Dr. C. D. Walcott centered his main efforts on the study of the Cambrian system, he conceived the idea of a monograph series, each of which should contain descriptions of all Cambrian fossils representing a major animal group. -
The Developmentof Early Imperial Dress from the Tetrachs to The
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Birmingham Research Archive, E-theses Repository University of Birmingham Research Archive e-theses repository This unpublished thesis/dissertation is copyright of the author and/or third parties. The intellectual property rights of the author or third parties in respect of this work are as defined by The Copyright Designs and Patents Act 1988 or as modified by any successor legislation. Any use made of information contained in this thesis/dissertation must be in accordance with that legislation and must be properly acknowledged. Further distribution or reproduction in any format is prohibited without the permission of the copyright holder. The Development of Early Imperial Dress from the Tetrarchs to the Herakleian Dynasty General Introduction The emperor, as head of state, was the most important and powerful individual in the land; his official portraits and to a lesser extent those of the empress were depicted throughout the realm. His image occurred most frequently on small items issued by government officials such as coins, market weights, seals, imperial standards, medallions displayed beside new consuls, and even on the inkwells of public officials. As a sign of their loyalty, his portrait sometimes appeared on the patches sown on his supporters’ garments, embossed on their shields and armour or even embellishing their jewelry. Among more expensive forms of art, the emperor’s portrait appeared in illuminated manuscripts, mosaics, and wall paintings such as murals and donor portraits. Several types of statues bore his likeness, including those worshiped as part of the imperial cult, examples erected by public 1 officials, and individual or family groupings placed in buildings, gardens and even harbours at the emperor’s personal expense. -
Catskill Trails, 9Th Edition, 2010 New York-New Jersey Trail Conference
Catskill Trails, 9th Edition, 2010 New York-New Jersey Trail Conference Index Feature Map (141N = North Lake Inset) Acra Point 141 Alder Creek 142, 144 Alder Lake 142, 144 Alder Lake Loop Trail 142, 144 Amber Lake 144 Andrus Hollow 142 Angle Creek 142 Arizona 141 Artists Rock 141N Ashland Pinnacle 147 Ashland Pinnacle State Forest 147 Ashley Falls 141, 141N Ashokan High Point 143 Ashokan High Point Trail 143 Ashokan Reservoir 143 Badman Cave 141N Baldwin Memorial Lean-To 141 Balsam Cap Mountain (3500+) 143 Balsam Lake 142, 143 Balsam Lake Mountain (3500+) 142 Balsam Lake Mountain Fire Tower 142 Balsam Lake Mountain Lean-To 142, 143 Balsam Lake Mountain Trail 142, 143 Balsam Lake Mountain Wild Forest 142, 143 Balsam Mountain 142 Balsam Mountain (3500+) 142 Bangle Hill 143 Barkaboom Mountain 142 Barkaboom Stream 144 Barlow Notch 147 Bastion Falls 141N Batavia Kill 141 Batavia Kill Lean-To 141 Batavia Kill Recreation Area 141 Batavia Kill Trail 141 Bear Hole Brook 143 Bear Kill 147 Bearpen Mountain (3500+) 145 Bearpen Mountain State Forest 145 Beaver Kill 141 Beaver Kill 142, 143, 144 Beaver Kill Range 143 p1 Beaver Kill Ridge 143 Beaver Meadow Lean-To 142 Beaver Pond 142 Beaverkill State Campground 144 Becker Hollow 141 Becker Hollow Trail 141 Beech Hill 144 Beech Mountain 144 Beech Mountain Nature Preserve 144 Beech Ridge Brook 145 Beecher Brook 142, 143 Beecher Lake 142 Beetree Hill 141 Belleayre Cross Country Ski Area 142 Belleayre Mountain 142 Belleayre Mountain Lean-To 142 Belleayre Ridge Trail 142 Belleayre Ski Center 142 Berry Brook -
Profiles of Colorado Roadless Areas
PROFILES OF COLORADO ROADLESS AREAS Prepared by the USDA Forest Service, Rocky Mountain Region July 23, 2008 INTENTIONALLY LEFT BLANK 2 3 TABLE OF CONTENTS ARAPAHO-ROOSEVELT NATIONAL FOREST ......................................................................................................10 Bard Creek (23,000 acres) .......................................................................................................................................10 Byers Peak (10,200 acres)........................................................................................................................................12 Cache la Poudre Adjacent Area (3,200 acres)..........................................................................................................13 Cherokee Park (7,600 acres) ....................................................................................................................................14 Comanche Peak Adjacent Areas A - H (45,200 acres).............................................................................................15 Copper Mountain (13,500 acres) .............................................................................................................................19 Crosier Mountain (7,200 acres) ...............................................................................................................................20 Gold Run (6,600 acres) ............................................................................................................................................21 -
Effect of Porphyritic Andesite Int Metamorphism Aureole in Sel
E-ISSN : 2541-5794 P-ISSN :2503-216X Journal of Geoscience, Engineering, Environment, and Technology Vol 5 No 2 2020 RESEARCH ARTICLE Effect of Porphyritic Andesite Intrusion on The Formation of Contact Metamorphism Aureole in Selo Gajah Hill Clastic Limestone, Bojonegoro Regency, East Java, Indonesia Tri Winarno1,*, Jenian Marin1, Wisnu Wijaya Jati1 1Department of Geological Engineering, Diponegoro University, Indonesia Corresponding author : [email protected] Telp :+62 857-4006-6835 Received: Nov 18, 2019, Accepted: Jun 25, 2020. DOI 10.25299/jgeet.2020.5.2.4098 Abstract At Selo Gajah Hill, Jari Village, Gondang Sub-district, Bojonegoro Regency, East Java there are limestone intruded by porphyritic andesite. The intrusion produces contact metamorphisms in the wall rocks. It is very interesting to study the protolith rock, facies of metamorphism and the zonation of contact metamorphism aureole. This research uses field observation method and laboratory analysis i.e. petrographic analysis. Field observation is conducted by doing geological mapping in the Bukit Selo Gajah area and rock sampling for petrographic analysis. Petrographic analysis aims to describe the texture of the rocks and the percentage of minerals, which will be used to determine the protolith rock, metamorphism facies and the determination of contact metamorphism zone. The lithology found in Mount Selo Gajah from oldest to youngest are clastic limestone with intercalation of marl, marl with intercalation of sandstone, porphyritic andesite intrusions, hornfels, and pyroclastic breccia. Metamorphic rocks on Selo Gajah Hill is the product of contact metamorphism of carbonate rock which was intruded by porphyritic andesite intrusion. The metamorphism facies found in the research area are hornblende hornfels and pyroxene hornfels with the protolith rock is carbonate rocks.