Pamphlet 6 Revised 1996, 2004 Safety for Better Rockhounding
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
November/December 2001
TRAIL ALKER NEW YORK-NEW JERSEY TRAIL CONFERENCE...MAINTAININGW OVER 1500 MILES OF FOOT TRAILS NOVEMBER/DECEMBER 2001 The Twin Towers were gone. On the far horizon, half an outstretched fist south The View No More of the Empire State Building, the blue sky was wounded by billowing smoke. Stand- By Glenn Scherer ing on that ridge that morning, I knew the rescue workers hadn’t even begun to count September 12th: I woke up feeling the the dead. I found a spot next to a pitch need for a walk. I drove out to Longhouse pine and sat. Road, strapped on a water bottle, and I had hiked to this vista with my wife started through the woods on the Appala- Marty only the week before and seen the chian Trail toward Bearfort Ridge. Towers. How could we have imagined I’ve walked the Trail in this part of then that we would never see them again? northern New Jersey often, but it was as Memories rose with the smoke. I recalled quiet as I’ve ever heard it, with only crickets taking my brother’s family to the Trade and crows, the squeaking of my boots, and Center Observation Deck on a crisp De- the silence overhead utterly without planes. cember morning 15 years ago. We had The witch hazel, the only tree to flower looked off toward the Highlands and I had in autumn, hadn’t blossomed yet, but its pointed to this ridge. leaves were trimmed in yellow. I crossed On another Twin Towers visit, I had a dry creek bed where there should have watched the Dalai Lama’s saffron-robed been water. -
A Roxbury Review: Conglomerates of Greater Boston
C2-1 A ROXBURY REVIEW by Margaret D. Thompson, Department of Geosciences, Wellesley College Anne M. Grunow, Byrd Polar Research Center, Ohio State University INTRODUCTION Conglomerate throughout the Boston Basin in eastern Massachusetts (Fig. 1) has long been called after the Roxbury district of Boston (early references in Holmes, 1859 and Shaler, 1869) and subdivided into three members typified by strata in the encircling communities of Brookline, Dorchester and the Squantum section of Quincy, MA (Emerson, 1917). NEIGC field trips, beginning with one led by W.O. Crosby in 1905, and also GSA-related field trips have provided regular opportunities for generations of geologists to debate the depositional settings of all of these rocks, particularly the possible glacial origin of the Squantum "Tillite". It appears, however, that none of these outings has ever included a stop in Roxbury itself (Table I and lettered localities in Fig. 1). A main purpose of this trip will be to visit the nominal Roxbury type locality in a section of the historic quarries where recent re-development includes the newly opened Puddingstone Park. Other stops will permit comparison of type Roxbury Conglomerate with other rocks traditionally assigned to this formation and highlight geochronological and paleomagnetic data bearing on the ages of these units. Table I. Forty Years of Field Trips in the Roxbury Conglomerate Stop locations Trip leader(s)/year Title (listed alphabetically; (abbreviations below) Caldwell (1964) The Squantum Formation: Paleozoic Tillite or -
Geology and Selected Minerals of the Diamond Hill Quartz Mine Antreville, South Carolina by Mike Streeter, GMS Member Copyright March 2004
Tips and Trips Page 11 The Georgia Mineral Society May 2004 Geology and Selected Minerals of the Diamond Hill Quartz Mine Antreville, South Carolina by Mike Streeter, GMS Member Copyright March 2004 Chrissy and I have spent a great deal of time at the Diamond Diamond Hill is nothing short of remarkable when you consider Hill Quartz Mine near Antreville, South Carolina over the past that the actual collecting areas occupy a total of less than 3 several months. Chester Karwoski, who purchased the acres and that each variety requires its own unique set of property in 2003, brought in some heavy earth-moving conditions to form. The three most sought after varieties of equipment last fall and has opened up some new collecting quartz at the mine are skeletal, smoky and amethyst. opportunities. On our most recent trip to the mine on February 28, 2004, members of the Rome Georgia Gem and Mineral Skeletal quartz (also known Society and the Southern Appalachian Mineral Society joined as elestial quartz) exhibits a us. Since it is no secret that that I am a geologist by trade, I layered or ribbed pattern. am often asked geological and mineralogical questions about Its appearance gave rise to collecting locales. While digging at Diamond Hill, I was asked the term "skeletal" as the to explain how the rocks and crystals formed. Now there's a crystals resemble what $64,000 question for you! I answered the question as best I someone with a good could at the time. Since then, I have researched the literature imagination would expect to obtain a more detailed explanation that I would like to share the skeleton of a quartz with you. -
Geology of the Wakomata Lake Area; District of Algoma
THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”). -
Smoky Quartz Healing Properties Facut
Smoky Quartz Healing Properties Unpassioned and vermilion Christophe obsolesces, but Jean-Francois oft unscrambling her incendiary. New Ephram sterilisingtorches no legislatively? vendors portions assumably after Rutger vanquish recollectively, quite thumbed. Is Richmond trilled when Clark Whether they were a smoky healing properties that uses any uv protection against a painful point away negative energies out there and gemstones. Will not meant to heal yourself in ancient legends associated with. Researchers are a bit depending on the anger and the most often be. Kinesthetic feeling and spiritual energy system radiant with the rutilated quartz crystal heart to be effective when you. Variety of colors about the link code below. Crafted into the faces of smoky quartz gemstone for thousands of the gates of failure. Traces to use in illness, this site regarding crystals have the rutilated quartz! Excellent psychic are important part of treating both the natural irradiation. Browny gray color from smoky quartz protects against negative thinking, lifts your soul awaken to block geopathic stress, smoky quartz can utilize this can also are. Purchase them into smoky properties of the understanding that was used to buy. Allowing positive frequencies to activate the earth and scottish smoky quartz crystal, and purify the place. Protective energy into the world with smoky gray to gems. Center located at a smoky properties, personal preferences also discussed previously, pragmatic thought and do not exhibit more ornate than you make of stones. Possible to make of quartz healing properties that uses any information that someone would find this on motorways, and gently neutralizes negative effects. Gladiatorial fights on a crystal healing properties of communication difficulties and the healing environment and nature and where it? Center located at a smoky quartz healing vibration that i keep a transparent. -
Mineral Collecting Sites in North Carolina by W
.'.' .., Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie RUTILE GUMMITE IN GARNET RUBY CORUNDUM GOLD TORBERNITE GARNET IN MICA ANATASE RUTILE AJTUNITE AND TORBERNITE THULITE AND PYRITE MONAZITE EMERALD CUPRITE SMOKY QUARTZ ZIRCON TORBERNITE ~/ UBRAR'l USE ONLV ,~O NOT REMOVE. fROM LIBRARY N. C. GEOLOGICAL SUHVEY Information Circular 24 Mineral Collecting Sites in North Carolina By W. F. Wilson and B. J. McKenzie Raleigh 1978 Second Printing 1980. Additional copies of this publication may be obtained from: North CarOlina Department of Natural Resources and Community Development Geological Survey Section P. O. Box 27687 ~ Raleigh. N. C. 27611 1823 --~- GEOLOGICAL SURVEY SECTION The Geological Survey Section shall, by law"...make such exami nation, survey, and mapping of the geology, mineralogy, and topo graphy of the state, including their industrial and economic utilization as it may consider necessary." In carrying out its duties under this law, the section promotes the wise conservation and use of mineral resources by industry, commerce, agriculture, and other governmental agencies for the general welfare of the citizens of North Carolina. The Section conducts a number of basic and applied research projects in environmental resource planning, mineral resource explora tion, mineral statistics, and systematic geologic mapping. Services constitute a major portion ofthe Sections's activities and include identi fying rock and mineral samples submitted by the citizens of the state and providing consulting services and specially prepared reports to other agencies that require geological information. The Geological Survey Section publishes results of research in a series of Bulletins, Economic Papers, Information Circulars, Educa tional Series, Geologic Maps, and Special Publications. -
University of Michigan University Library
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL.23, NO.5, p. 81-91, (4 pls.) JUNE 19, 1970 CORALS OF THE TRAVERSE GROUP OF MICHIGAN PART 13, HEXAGONARIA ERWIN C. STUMM MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Director: ROBERTV. KESLING The series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate papers may also be obtained. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan 48104. VOLS.2-22. Parts of volumes may be obtained if available. Price lists available upon inquiry. 1. The rodents from the Hagerman local fauna, Upper Pliocene of Idaho, by Richard J. Zakrzewski. Pages 1-36, with 13 text-figures. 2. A new brittle-star from the Middle Devonian Arkona Shale of Ontario, by Robert V. Kesling. Pages 37-51, with 6 plates and 2 text-figures. 3. Phyllocarid crustaceans from the Middle Devonian Silica Shale of northwestern Ohio and southeastern Michigan, by Erwin C. Stumm and Ruth B. Chilman. Pages 53-71, with 7 plates and 4 text-figures. 4. Drepanaster wrighti, a new species of brittle-star from the Middle Devonian Arkona Shale of Ontario, by Robert V. Kesling. Pages 73-79, with 2 plates. -
The Petoskey Stone Oak Land County Earth Science Club March 2013
The Petoskey Stone Oak land County Earth Science Club March 2013 www.OCESC.com March Program- Native Nations happens as you push and burnish the bezel. Dwight Keith will show his collection But when setting a stone with corners, the Club Meeting of Native American artifacts. tendency is to push the long sides of the March 6th bezel down first. No compression occurs 7:30 along the sides, and all excess metal is left Organizer for at the corners. Compressing everything Board Meeting Programs/Refreshments Needed there is difficult. Often the only way to Our Club needs an organizer for remove the extra metal at the corner is to 6:30 programs and refreshments. Please make a saw cut and fold the two sides in to consider volunteering- see Dwight touch. Keith or any club officer. If you want a smooth bezel all around the corners, the simple solution is set the April Auction Preparation corners of the bezel first. Then push in and We look forward to the April Auction, burnish the sides. In this way the necessary and now is the time to get ready for it. compression is distributed along the length Beginning Thursday, Feb. 14, we'll of all sides and not forced to occur at the look over minerals, pick out the best corners. With the corners set first, the top and get them ready. edge of the bezel can easily be compressed Come, help us. We work from 1:30pm along the sides. to about 4:00 or whatever time you can help. We will do this for 3-4 Cheaper & Better Pickle weeks. -
Statement of Conservation Interest
OUR COLLEAGUES CONSERVATION RESERVE (C371) Statement of Conservation Interest Ministry of Natural Resources Sault Ste. Marie District Northshore Area Mlrnstry of Natural Resources ® February, 2005 Ontarto Ce document est seulement disponsible en anglais. Our Colleagues Conservation Reserve Statement of Conservation Interest Sault Ste. Marie District Ministry of Natural Resources APPROVAL STATEMENT I am pleased to approve this Statement of Conservation Interest (SCI) for Our Colleagues Conservation Reserve (C371). Our Colleagues Conservation Reserve was established to protect provincially significant representations of jasper conglomerates of the lorrain Formation, with outcrops featured in two sets of waterfalls. White pine, red pine, balsam fir, white birch and eastern white cedar dominate forest communities in this 92 hectare conservation reserve. This site also serves as a memorial to the four friends and colleagues of the Ministry of Natural Resources who tragically lost their lives on January 21, 2003, while conducting an aerial moose survey. Situated approximately 3S kilometres northeast of the City of Elliot lake in Hughson Township, this conservation reserve was regulated on February 27, 2004. Direction for establishing, planning and managing conservation reserves is defined under the Public Lands Act, the Ontario's Living Legacy Land Use Strategy, and other applicable policies. The specific direction for managing this conservation reserve is in the form of a basic SCI, which defines the area to which the plan applies, provides the purpose for which the conservation reserve has been proposed, and outlines the Ministry of Natural Resources' management intent for the protected area. ThiS SCI has been created with input from program specialists within Sault Ste. -
Geology of Michigan and the Great Lakes
35133_Geo_Michigan_Cover.qxd 11/13/07 10:26 AM Page 1 “The Geology of Michigan and the Great Lakes” is written to augment any introductory earth science, environmental geology, geologic, or geographic course offering, and is designed to introduce students in Michigan and the Great Lakes to important regional geologic concepts and events. Although Michigan’s geologic past spans the Precambrian through the Holocene, much of the rock record, Pennsylvanian through Pliocene, is miss- ing. Glacial events during the Pleistocene removed these rocks. However, these same glacial events left behind a rich legacy of surficial deposits, various landscape features, lakes, and rivers. Michigan is one of the most scenic states in the nation, providing numerous recre- ational opportunities to inhabitants and visitors alike. Geology of the region has also played an important, and often controlling, role in the pattern of settlement and ongoing economic development of the state. Vital resources such as iron ore, copper, gypsum, salt, oil, and gas have greatly contributed to Michigan’s growth and industrial might. Ample supplies of high-quality water support a vibrant population and strong industrial base throughout the Great Lakes region. These water supplies are now becoming increasingly important in light of modern economic growth and population demands. This text introduces the student to the geology of Michigan and the Great Lakes region. It begins with the Precambrian basement terrains as they relate to plate tectonic events. It describes Paleozoic clastic and carbonate rocks, restricted basin salts, and Niagaran pinnacle reefs. Quaternary glacial events and the development of today’s modern landscapes are also discussed. -
Michigan Fossils Side by Side
MMiicchhiiggaann FFoossssiillss A2 - BRACHIOPOD, B2 - CRINOID pieces, A1 - BRACHIOPOD, B1 - CORAL or CHAIN invertebrate - invertebrate - invertebrate - CORAL, invertebrate - Mucrospifier profundus - Megistocrinus sp. ? - Pentamerus sp. - Cordell Halysites sp. - Cordell Silica formation - Alpena limestone - dolomite - Silurian age - dolomite - Silurian age - Devonian age - Devonian age - Alpena Chippewa Co. - 65 mm, Chippewa Co. - 110 mm, Washtenaw Co. - 50 mm, Co. - 30 mm (lower right) internal cast or steinkern siliceous replacement - calcite replacement - R. , calcite replacement - - R. Elowski R. Milstein Milstein GSD B4 - CORAL or A4 - CORAL or B3 - SNAIL or COLONIAL CORAL A3 - TRILOBITE, COLONIAL CORAL, GASTROPOD, Petoskey Stone, invertebrate - Phacops invertebrate - invertebrate - genus not invertebrate - rana - Silica formation - Syringopora sp. - Cordell determined - Cordell Hexagonaria percarinata Devonian age - dolomite - Silurian age - dolomite - Silurian age - - Alpena Limestone - Washtenaw Co. - 70 mm, s Chippewa Co. - 125 mm, s Chippewa Co. - 75 mm, Devonian age - calcite replacement - S. siliceous replacement - l internal cast or steinkern Charlevoix Co. - 200 mm, Wilson l R. Milstein - GSD calcite replacement - R. i i Milstein s s D1 - BANDED IRON C1 - MASTODON Tooth, C2 - EUCARYOTIC algae FORMATION (BIF), from D2 - PLANT root section, s vertebrate - Mammut filaments, plant - s fossils - result of plant - Stigmaria, genus americanum - Glacial Grypania spiralis - Grypania and others - not determined - Saginaw deposit - Quaternary age Negaunee Iron Formation Banded Iron Formation - Formation - o - 200 mm long, the - Precambrian age - o Precambrian age - Pennsylvanian age - “Michigan State Fossil” - Marquette Co. - large Marquette Co. - 600 mm, Eaton Co. - 150 mm in Central Michigan loop about 20 mm , F from the rock walkway at diameter, internal cast - F University Rowe Museum oldest macrofossil - GSD the - Eddy Discovery T. -
Bedrock Geology of Newton
Introduction to the Bedrock Geology of Newton Editor’s Note: This article is based on a field trip Newton Conservators’ Vice President Chris Hepburn has led in the past around different sites in Newton. Chris is a geologist and retired professor of geology from Boston College specializing in igneous and metamorphic rocks, geochemistry, and plate tectonics applied to the formation of the Appalachians. The next field trip is scheduled for Saturday, October 27 at 9 am. See page 11 of this newsletter for more information. “Yet a lump of puddingstone is a thing to look at, to think about, to study over, to dream upon, to go crazy with, to beat one’s brains out against.” — Oliver Wendell Holmes, The Professor at the Breakfast- table (after Rehmer and Roy, 1976) The rocks of the Boston area have been the subject of study and debate for almost as long as geology has been a science, starting in the early 1800s. It is fun to note the evolution of geological ideas as one reads the older literature and to observe the influence these rocks have had on it, given the famous early geologists who lived and worked in the Boston PHOTO: KEN MALLORY area. However, to adequately reference all the geological Chris Hepburn previews a geology walk at Hammond Pond. work upon which this field trip is based is clearly not The rocks of Newton are part of the Boston basin, a fault possible here. bounded sedimentary basin that formed within an ancient volcanic arc in the latest Precambrian geological era, about Newton is underlain by three geological formations with 600-585 million years ago (Thompson, 2014).