2 edition of Geology of the Coromandel region found in the catalog.
Geology of the Coromandel region
Bruce Newton Thompson
Bibliography: p. 22.
|Statement||[by] B. N. Thompson.|
|Series||Report NZGS ;, 14|
|LC Classifications||QE342 .A792 no. 14|
|The Physical Object|
|Pagination||ii, 22 p.|
|Number of Pages||22|
|LC Control Number||70387243|
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An illustration of a " floppy disk. The geology of the Coromandel subdivision, Hauraki, Auckland Item Preview remove-circle Share or Embed This Item. ISBN: OCLC Number: Notes: "A companion publication, Teachers resources guide, number 1 is also available from the publishers"--Foreword.
An account is given of the early geological exploration and mining history of the Coromandel Goldfield. The writer's interpretation of the basement and igneous geology, and of the metallogenesis of gold-silver and base metal ores has resulted in radical by: 7.
Abstract: The Coromandel Harbour map region consists of a Neogene volcanic sequence overlying a late Jurassic sedimentary basement. Both host epithermal vein systems from which over oz (> kg) of gold bullion with high silver content were produced.
Coromandel region where post-main-rhyolite, pre-mineralisation andesitic (intrusive) units have not elsewhere been recognised. Most of the area away from the gorge is blanketed by a layer.
Andesitic lavas, rudites, and finer sediments of the Coromandel Group were erupted during the lowermost Pliocene. They are conformably overlain by rhyolitic sediments, ignimbrites, and minor lavas. The Table Mountain area (N49) is a region of steepJy dissected andesitic, rhyolitic, and associated sedimentary deposits belonging to three groups.
Andesitic lavas, rudites, and finer sediments of the Coromandel Group were erupted during the lower-most Pliocene. They are conformably overlain by rhyolitic sediments, ignimbrites, and.
The base rock of the Coromandel Peninsula is greywacke, a sedimentary rock deposited on the sea floor about million years ago. Its later uplift and folding formed the Coromandel Range and the peninsula’s general shape.
Greywacke is exposed only in parts between Tapu and Cape Colville; it is overlain elsewhere by more recent volcanic rocks. The Coromandel Peninsula on the North Island of New Zealand extends 85 kilometres north from the western end of the Bay of Plenty, forming a natural barrier protecting the Hauraki Gulf and the Firth of Thames in the west from the Pacific Ocean to the east.
It is 40 kilometres wide at its broadest point. The intention of this book is to provide a useful and informative introduction to the variety of geology in the local region. It showcases the information held on geological sites at BRERC, and the work of many local experts.
At the end of the book there is information on the many local groups and organisations for people with a common interest. Geological Guide - South Greenland. The Narsarsuaq - Narsaq - Qaqortoq region.
This book is a handy guide book to the fascinating geology of South Greenland which houses some world-famous mineral localities. It focuses on the description of the main geological features of the region and of localities and is planned as a handy guide book to be used in the field.
ISBN: OCLC Number: Notes: Panel title. Includes text, ill. and ancillary maps. Issued in pocket of explanatory book. About this book Published by the American Geophysical Union as part of the Field Trip Guidebooks Series, Volume The San Francisco Bay region is one of the premier sites in the world to see the effects on land of plate tectonics.
Abstract The Table Mountain area (N49) is a region of steeply dissected andesitic, rhyolitic, and associated sedimentary deposits belonging to three groups. Andesitic lavas, rudites, and finer sediments of the Coromandel Group were erupted during the lowermost Pliocene.
They are conformably overlain by rhyolitic sediments, ignimbrites, and minor lavas of the lower to mid-Pliocene. New Zealand Coromandel Geology Tour - Kindle edition by John Eric Edinger, Linda Price. Download it once and read it on your Kindle device, PC, phones or tablets.
Use features like bookmarks, note taking and highlighting while reading New Zealand Coromandel Geology : John Eric Edinger, Linda Price. English, Book, Illustrated, Government publication edition: The geology of the Coromandel Subdivision, Hauraki, Auckland / by Colin Fraser ; assisted.
Relates the physical and geometric elegance of geologic structures within the Earths crust and the ways in which these structures reflect the nature and origin of crystal deformation through time.
The main thrust is on applications in regional tectonics, exploration geology, active tectonics and geohydrology. Techniques, experiments, and calculations are described in detail, with the purpose.
Lexington, KY (Ap ) – One of the most popular books published by the Kentucky Geological Survey (KGS) at the University of Kentucky has been updated for publication of a second ing the Geology of the Cincinnati/Northern Kentucky Region, written by University of Cincinnati geology professor emeritus Paul E.
Potter, was first published in geology of the Arabian Peninsula. Each author prepared a description of the geology of the area for which he was responsible, as shown in the sources of geologic compilation diagram on the peninsular map.
The U.S. Geological Survey undertook the publishing of the volume. This book describes to travellers, the general public and beginners in geology in New Zealand something of the tremendous variety of our rocks, minerals and fossils and describes what to look for.
Wellington Region (42,) Book reviews (36,) Poetry (28,) Periodicals (27,) Earthquakes -- Christchurch (26,) History (24,) Geology--Coromandel Peninsula Geology--Coromandel Peninsula; Filter By Type All Results Reference sources (16) Filter by.
Coromandel Gold is a well-illustrated practical guide to 13 of the historic goldfields of Coromandel Peninsula. Its superb colour photos, by landscape photographer Lloyd Homer, are complemented by numerous black and white images, maps and : Phil Moore, Neville Ritchie.
Edbrooke, S.W. Geology of the Auckland area. Lower Hutt: Institute of Geological & Nuclear Sciences Limited. Institute of Geological & Nuclear Sciencesgeological map 3 74 p. + 1 fold.
map. Abstract: The Aucklandgeological map cov km 2 of the greater Auckland area, parts of southern Northland and northern Waikato, and Coromandel Peninsula, in the north of. This book brings together in one place as much factual data as possible relating to the engineering geology of the Sydney Region, A huge amount of information resides in the files of various consulting and government organizations from the innumerable site.
The Hauraki goldfield in the Coromandel volcanic zone contains approximately 50 adularia-sericite epithermal Au-Ag deposits in a km-long by km-wide north-south-trending belt. These deposits have produced approximatelykg Au and Mkg Ag and formed from Miocene to Pliocene subaerial hydrothermal systems.
Geology of the Central Copper River Region, Alaska Volume 41 of Geological Survey professional paper Geology of the Central Copper River Region, Alaska, Walter Curran Mendenhall Professional paper Volume 48 of Series A--Economic geology Volume 60 of Series B--Descriptive geology: Author: Walter Curran Mendenhall: Publisher: U.S.
Government. Geology of the National Capital Region: Field Trip Guidebook. Scott Southworth, William Chapin Burton. U.S. Geological Survey, - Geology - pages. 1 Review.
Preview this book» What people are saying - Write a review. User Review - Flag as inappropriate. This was a very useful book.
Many thanks. Selected pages. Page Page 5/5(1). Sheet QM Coromandel: geological resource map of New Zealand, / A.B. Chris Date: From: Lower Hutt, N.Z.: Institute of Geological & Nuclear Sciences, c Geological map of Coromandel survey district [cartographic material] / compiled and dra.
Geology and Post-Cretaceous Sedimentary Distribution Deposits of Coromandel (MG) Southern Region Diamatiferous Deposits. Geology of the Coromandel Harbour area. 44 p. Skinner, D N B, $50 Gm4: Geology of the Rai Valley area. 44 p. Johnston, M R, $50 Gm5: Geology of the middle reaches of the Mohaka River.
38 p. Cutten, H N C, $50 Gm6: Geology of the Otago schist and adjacent rocks. (Map only) Mortimer, N $30 Gm7. Identifier: geologyofcoroman00fras Title: The geology of the Coromandel subdivision, Hauraki, Auckland Year: (s) Authors: Fraser, Colin, Adams, James Henry New Zealand Geological Survey Subjects: Geology Publisher: Wellington, N.Z.: by authority John Mackay, Govt.
Printer Contributing Library: University of Connecticut Libraries Digitizing Sponsor: LYRASIS Views: The Auckland Region of New Zealand is built on a basement of greywacke rocks that form many of the islands in the Hauraki Gulf, the Hunua Ranges, and land south of Port Waitākere Ranges in the west are the remains of a large andesitic volcano, and Great Barrier Island was formed by the northern end of the Coromandel Volcanic Zone.
The main isthmus and North Shore are composed of. Geology of the Prince William Sound and Kenai Peninsula Region, Alaska Compiled by Frederic H. Wilson and Chad P. Hults. Abstract. The Prince William Sound and Kenai Peninsula region includes a significant part of one of the world’s largest accretionary complexes and a small part of the classic magmatic arc geology of the Alaska Peninsula.
Jolly parades to be held across Hauraki-Coromandel region 2 Dec, PM 2 minutes to read Don Law on his tractor from a previous Whangamata Christmas Parade. ⓘ Owera Mine, Whangapoua, Coromandel peninsula, Thames-Coromandel District, Waikato Region, New Zealand Mineral and/or Locality is an outreach project of the Hudson Institute of Mineralogy, a (c)(3) not-for-profit organization.
The geology of diamonds in Brazil is briefly summarized in relation to the known primary source localities and secondary host rocks.
Emphasis is placed on the geotectonic control of mineralized primary diamond source rocks and it is shown that the distribution and occurrences in Brazil of diamond-bearing versus nondiamond-bearing kimberlites and/or lamproites are compatible with the.
Surficial Geology and Neotectonics of Selected Areas of Western Idaho and Northeastern Oregon By Stephen F. Personius INTRODUCTION The region described in diis report is in an area of complex geology and geomorphology in west ern Idaho and northeastern Oregon (fig.
The western part of the region is underlain by rocks comAuthor: S.F. Personius. Geology and Mineralisation of the Monowai Mine Coromandel Peninsula, P.
ROBERTS. in Mineral Deposits of New Zealand, Ed Dr. D Kear. ⓘ Paroquet Mine Bell, J.M., Fraser, C. () The geology of the Waihi-Tairua Subdivision, Hauraki Division. Geology of the Anlauf and Drain quadrangles, Douglas and Lane Counties, Oregon: USGS Bulletin D,62 pp. plus 2 plates in pocket.
Very good condition. Geology and coal deposits in part of the Coos Bay coal field, Oregon: USGS Bulletin B,21 pp. plus 4 Seller Rating: % positive. To follow the text discussions of each e-book chapter, see the Table of Contents.
Cover graphic. Airliner view of the Outer NY Harbor at the mouth of the New York Bight. Figure 1. Map of the greater New York City region. Figure 2. Major cities and interstate highways in the New York City region. Figure 3. Shaded relief map (digital elevation.
RECONNAISSANCE GEOLOGY OF THE AS SULAYMI QUADRANGLE SHEET 26/41C, KINGDOM OF SAUDI ARABIA By I/ James E. Quick ABSTRACT X The As Sulaymi quadrangle, located in the Arabian Shield between lat 26°00' and 26°30' N.
and long 41°00' and 41°30' E., is underlain by three volcano-sedimentary units and a wide range. Vol. Suppe J. GEOLOGY OF THE LEECH LAKE MOUNTAIN- BALL MOUNTAIN REGION CALIFORNIA wps, light wear, vg, 82 pp., 12 plts, 23 figs.
Price: $ (stock#UC) Vol. Givens C. R. EOCENE MOLLUSCAN BIOSTRATIGRAPHY OF THE PINE MOUNTAIN AREA VENTURA COUNTY CALIFORNIA wps light wear, vg, pp. 11 plts.Geology of the Kelowna Area and Origin of the Okanagan Valley, British Columbia book.
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