Pamphlet 4: Collecting Minerals in Michigan
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Geology Club Mineral: Collecting Trip
Geology Club: Mineral Collecting Trip (10 October 2009) Trip Notes by Charles Merguerian STOP 1 – Grossular Garnet Locality, West Redding, Connecticut. [UTM Coordinates: 630.71E / 4575.38N, Bethel quadrangle]. Covering roughly 60 acres of land, this enigmatic massive fine-grained grossularite garnet + diopside rock in West Redding has made many mineral collectors and geologists take notice. Walk up the steep slope east of Simpaug Turnpike to see highly fractured, massive cinnamon-colored grossular garnet rock, part of a 0.6-km wide heart-shaped mass found at the faulted contact between the Stockbridge Marble (OCs) and injected muscovitic schist of the Rowe Schist member (OCr) of the Hartland Formation (Figure 1). According to Rodgers et al. (1985), we are very near Cameron’s Line (red and black line in Figure 1). Figure 1 – Geologic map of the area surrounding Stop 1 showing the Proterozoic gneissic rocks (Yg) and Cambrian Dalton Schist (Cd) to the west, the Stockbridge Marble (OCs), Cameron’s Line (CL in red), the injected schistose rocks of the Rowe Formation (OCr), and an Ordovician granitoid (Og) that may be responsible for this unusual Ca++-enriched skarn deposit. Note the NW-trending high-angle brittle faults that cut the region. (Adapted from Rodgers et al. 1985.) Two knolls at this locality are almost entirely composed of grossularite garnet (var. essonite) and lesser clinopyroxene. Mostly the garnet occurs alone with minor quartz and localized quartz veining has been observed. Chemical analysis of the garnet (SiO2 = 39.10%, CaO = 34.85%, Al2O3 = 19.61%, and total FeO+Fe2O3 = 5.44%), are quite similar to published analyses of grossular garnet, including the phenomenal grossular garnet crystals from Morelos, Mexico. -
Symposium on Agate and Cryptocrystalline Quartz
Symposium on Agate and Cryptocrystalline Quartz September 10 – 13, 2005 Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter; Colorado School of Mines Geology Museum; and U.S. Geological Survey 2 Cover Photos {top left} Fortification agate, Hinsdale County, Colorado, collection of the Geology Museum, Colorado School of Mines. Coloration of alternating concentric bands is due to infiltration of Fe with groundwater into the porous chalcedony layers, leaving the impermeable chalcedony bands uncolored (white): ground water was introduced via the symmetric fractures, evidenced by darker brown hues along the orthogonal lines. Specimen about 4 inches across; photo Dan Kile. {lower left} Photomicrograph showing, in crossed-polarized light, a rhyolite thunder egg shell (lower left) a fibrous phase of silica, opal-CTLS (appearing as a layer of tan fibers bordering the rhyolite cavity wall), and spherulitic and radiating fibrous forms of chalcedony. Field of view approximately 4.8 mm high; photo Dan Kile. {center right} Photomicrograph of the same field of view, but with a 1 λ (first-order red) waveplate inserted to illustrate the length-fast nature of the chalcedony (yellow-orange) and the length-slow character of the opal CTLS (blue). Field of view about 4.8 mm high; photo Dan Kile. Copyright of articles and photographs is retained by authors and Friends of Mineralogy, Colorado Chapter; reproduction by electronic or other means without permission is prohibited 3 Symposium on Agate and Cryptocrystalline Quartz Program and Abstracts September 10 – 13, 2005 Editors Daniel Kile Thomas Michalski Peter Modreski Held at Green Center, Colorado School of Mines Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter Colorado School of Mines Geology Museum U.S. -
Maine the Way Life Should Be. Mineral Collecting
MAINE The Way Life Should Be. Mineral Collecting The Maine Publicity Bureau, Inc. Quarries You May Visit # 1 Topsham: The Fisher Quarry is located off Route 24 in Topsham. This locale is best known for crystals of topaz, green microlite, and dark blue tourmaline. It has also produced other minerals such as beryl, uraninite and cassiterite. #2 Machiasport: At an area known as Jasper Beach there is an abundance of vari-colored jasper and/or rhyolite specimens. Located on Route 92. #3 Buckfield: The Bennett Quarry, located between Buckfield and Paris Hill, has produced fine specimens of blue and pink beryl including some gem material. It is also known for crystals of quartz, green tourmaline and rare minerals. #4 Casco: The Chute Prospect is best known for vesuvianite. It is located east of Route 302-35. Crystals of “cinnamon” garnet, quartz and pyrite are also found here. #5 Georgetown: The Consolidated Feldspar Quarry has produced excel lent specimens of gem citrine quartz, tourmaline and spodumene. Rose Quartz, cookeite and garnet are also found. #6 Paris: Mount Mica is world famous for tourmaline and this gem material was discovered here in 1821. This is one of the most likely places for a collector to find tourmaline. Mount Mica has produced a host of other minerals including beryl, cookeite, black tourmaline, colum- bite, lepidolite and garnet. (Currently being mined) #7 Greenwood: The Tamminen Quarry and the Harvard Quarry, both located near Route 219, have produced an interesting variety of miner als. The Tamminen Quarry is best known for pseudo-cubic quartz crystals, montmorillonite, spodumene and garnet. -
Origin of Fibrosity and Banding in Agates from Flood Basalts: American Journal of Science, V
Agates: a literature review and Electron Backscatter Diffraction study of Lake Superior agates Timothy J. Beaster Senior Integrative Exercise March 9, 2005 Submitted in partial fulfillment of the requirements for a Bachelor of Arts degree from Carleton College, Northfield, Minnesota. 2 Table of Contents AGATES: A LITERATURE REVEW………………………………………...……..3 Introduction………………....………………………………………………….4 Structural and compositional description of agates………………..………..6 Some problems concerning agate genesis………………………..…………..11 Silica Sources…………………………………………..………………11 Method of Deposition………………………………………………….13 Temperature of Formation…………………………………………….16 Age of Agates…………………………………………………………..17 LAKE SUPERIOR AGATES: AN ELECTRON BACKSCATTER DIFFRACTION (EBSD) ANALYSIS …………………………………………………………………..19 Abstract………………………………………………………………………...19 Introduction……………………………………………………………………19 Geologic setting………………………………………………………………...20 Methods……………………………………………………...…………………20 Results………………………………………………………….………………22 Discussion………………………………………………………………………26 Conclusions………………………………………………….…………………26 Acknowledgments……………………………………………………..………………28 References………………………………………………………………..……………28 3 Agates: a literature review and Electron Backscatter Diffraction study of Lake Superior agates Timothy J. Beaster Carleton College Senior Integrative Exercise March 9, 2005 Advisor: Cam Davidson 4 AGATES: A LITERATURE REVEW Introduction Agates, valued as semiprecious gemstones for their colorful, intricate banding, (Fig.1) are microcrystalline quartz nodules found in veins and cavities -
The Lake Superior Agate
Minnesota Gem: The Lake Superior Agate Its wide distribution and iron-rich bands of color reflect the state gemstone's geologic history in Minnesota Scott F. Wolter N 1969 the dream of Mrs. Jean it was the best choice. The agate IDahlberg was realized: The Lake reflects many aspects of Minnesota. Superior agate was designated by the It was formed during violent, fiery lava Minnesota Legislature as the official eruptions that occurred in our state state gemstone. about a billion years ago. The stone's The late Mrs. Dahlberg, long-time predominant red color comes from rock hound and ardent fan of the agate, iron, the major industrial mineral in testified before the state legislative our state. Finally, the widely distrib- committee considering the bill. She uted agate reveals the impact of gla- knew how perfect the Lake Superior cial movement across Minnesota agate was for the state gemstone. 10,000 to 15,000 years ago. However, there were other logical The Lake Superior agate is inti- candidates. The brazen red Bing- mately related to two prominent geo- hamite and blazing yellow silkstone, logic features of Minnesota: the both iron-rich jaspers found in the majestic and rugged lava flows Cuyuna iron range area, were logical exposed along the shoreline of Lake selections. Thompsonite, the beau- Superior and the lake-freckled glacial tiful and popular zeolite mineral found debris that covers nearly all the state. only in Minnesota on an isolated More than a billion years ago, the stretch along Lake Superior, was North American continent began to another strong candidate. -
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. -
General Information- Michigan's Gem Stones
CONTENTS: INDUSTRIES MAP —————— FACING I GENERAL INFORMATION- —————— I MICHIGAN'S GEM STONES- —————— 4 ASSAYS AND TESTS———— ————— I I ARTICLES, PERIODICALS, BOOKS- —————12 SOCIETIES—————————————————— ———— 23 MUSEUMS—————————————————— ———— 26 GEOLOGIC TIME SCALE ———— 30 GEOLOGIC MAP —————— ————— 3 I NMICHIGAN DEPARTMENT OF CONSERVATION ^GEOLOGICAL SURVEY DIVISION FREE DISTRIBUTION ONLY PREFACE TO THIRD EDITION The first edition, published in April, 1958 was needed in responding to queries following a mineral show on the Depart- ment T-V program "Michigan Conservation11. The second edition, July, 1959) was characterized by the addition of the section on gem stones* An abstracted version of the second edition titled "Pebbles to Pendants" was published in the July, 1958 issue of "Michigan Conservation". The present 'third edition is another major revision. Among the new materials added are: l) bedrock geologic map, 2) mineral industries map, 3) rock column and time scale, 4) mineral and fossil sketches, and 5) locality sketch maps* These, along with the cover, were prepared by Jim Campbell of our staff. The book list has been expanded and several titles were added to the articles list. Suggestions received from Arthur Johnstone, of the Michigan Mineralogical Society, were particularly helpful. Information regarding mineral and lapidary businesses may be found in the appropriate advertising media as well as from many of the clubs. Robert W. Kelley, Geologist Geological Survey Division Michigan Dept. Conservation March, I960 Lansing MICHIGAN'S MIN ERAL EXTRACTING INDUSTRIES D NON-METALLIC B BRINE H SALT 0 CLAY 0 SHALE 9 DOLOMITE H LIMESTONE 13 SAND& GRAVELCPRINCIPAL AREA) H GLASS SAND 0 GYPSUM B SANDSTONE D MARLCPRINCIPAL AREA) B PEAT • MISCELLANEOUS STONE A METALLIC L COPPER A IRON O FUELS <D GAS • OIL MAJOR FIELDS € OIL & GAS INDIANA O H I O GENERAL INFORMATION INTRODUCTION Interest in collecting minerals and gem stones and in doing lapidary work certainly is on the increase today. -
ROCK TALK Fax: 520-322-6031 E-Mail: [email protected] January – February 2012 Website: Volume 6, Issue 3
Tucson Gem and Mineral Society, Inc. PO Box, 42588, Tucson, Arizona 85733 Ph: 520-322-5773 ROCK TALK Fax: 520-322-6031 E-mail: [email protected] January – February 2012 Website: www.tgms.org Volume 6, Issue 3 President’s Page President’s Page … CONTINUED Greetings to all of our members and those members that contributed with hoping you had a wonderful Holiday donations to the Community Food Bank and Season with your friends and family. the Tucson Firefighters Toy Drive. This is an Lots of love, fun and food to remind attempt to, not only help the families of us of how fortunate we are and how Tucson, but give the Tucson Gem and Mineral Society a positive image in our community. much we appreciate each other and all our blessings. Now we This is so important to our being considered have a New Year approaching and an important part of Tucson, we are more a time of renewal and resolutions. than a Show, we are a responsible and viable Time to reflect and get busy in 2012. resource that can and should be appreciated We have a lot to do. all year. The Show is fast approaching and our volunteers So, the New Year is upon us, lets learn from and staff are hard at work just trying to get the past and take that knowledge into the everything ready for one of the best Shows we future to make better choices and decisions. have ever sponsored. “Minerals of Arizona” Thank you all for being a part of our Society promises to bring to our visitors and dealers an and now, lets "get on with the Show!!!!” opportunity to be a part of a very special event. -
Thunder Bay Agate Mine
Thunder Bay Agate Mine Last Spring I lead a group of undergraduate geology students around Lake Superior. One of the best stops we had was at the Thunder Bay Agate Mine. As it is right on the way to the better-known amethyst mines, I'd recommend all headed up that way stop for a visit. The mine is a dig-your-own fee area. It is located just a few miles north of Thunder Bay, just north-east of the Terry Fox Monument (another place that is worth a stop). A mile or so east of the monument on Hwy. 11-17, turn left on highway 527. There is an agate mine sign at the intersection, so it is hard to miss. The mine is about 1/2 mile up 527, on the left. That turn off is also well marked. There is a big parking area by their shop. You can walk or drive down a short distance down a well maintained dirt road to the mine from there. We were greeted and given a tour of the shop and the deposit. The students then got to go to work. The fee is $8 per pound, with the price pro-rated to reflect the poundage of agate rather than the surrounding matrix. There is a reduced rate for clubs. There was agate all over the place, and it could be collected without much in the way of tools. If you want to pound, well, there was opportunity for that too. The agate is a seam or vein agate, formed in brecciated iron carbonate of the Proterozoic Gunflint Formation. -
General Meeting Thursday, September 20, 2012 7:00 P.M
June - September, 2012 Volume 44, No. 1, Page 1 General Meeting Thursday, September 20, 2012 7:00 p.m. Location: Clubhouse, 4619 69th Street North, St. Petersburg, FL Bring in items you collected over the summer, or what you have made. Did you go to a mineral mine out of state? Tell us about it! Special Presentation by Tom Smith Professional Gem and Diamond Cutter www.adamasfacet.com It’s September and DUES ARE DUE once again. Please give them to the membership chair- person, or Jerry Heer, Treasurer at our General Meeting. DUES ARE DUE! $15.00 Individuals—$20 per family If your last name starts with A-M, please bring goodies to our meeting to share. Page 2 Rock-A-Gram June-September, 2012 Board Members Julia Larson, President . ... ... .. .. ... 727-522-1254 Pat Davis, 3 Year Director/ Email: [email protected] Past President . .......... .. ... ... .. .. ... 727-323-2147 Email: [email protected] Dave Schwebel, Vice President .. ... 727-547-0364 Email: [email protected] Dave Kane, 2 yr. Director ... .. .. ... 727-799-2352 Email: [email protected] Jerry Heer, Treasurer .. ... ... .. .. ... 419-344-9999 Email: [email protected] Dave Watson, 1 yr. Director . .. .. ... 727-541-2917 Email: [email protected] Stephen Redden, Recording Secretary 727-546-2052 Email: [email protected] Bucky Joseph, 1 yr. Director .. .. ... 727-252-8142 Email: [email protected] Donna Sapp, Correspondence Debbie Bremer, Editor . ... ... .. .. 727-298-0061 Secretary . ... ... .. ... ... .. ... ... .. .. ... 727-420-0383 Rock-A-Gram Newsletter Email: [email protected] Email: [email protected] SGAMS Clubhouse Address: 4619 69th Street North, St. Petersburg, FL 33709, www.sgams.com Clubhouse Activities: Listed on mailer coversheet and announced at membership meetings. -
USGS Bulletin 1309 the Geologic Story of Isle Royale National Park
Norman King Huber The geologic story of Isle Royale National Park United States Geological Survey Bulletin 1309 (1975) CONTENTS The island in history ------------------------------------------ 2 A look at the landscape -------------------------------------- 5 The building blocks-rocks and minerals ---------------------- 8 Volcanic rocks ---------------------------------------------- 8 Sedimentary rocks------------------------------------------ 13 Pyroclastic rocks -------------------------------------------- 14 The way the rocks are stacked up --------------------------- 14 A volcanic pile-the Portage Lake Volcanics ----------------- 14 Rock Harbor-Tobin Harbor area --------------------------- 17 Washington Harbor area------------------------------------ 20 An ancient alluvial fan-the Copper Harbor Conglomerate ---------------------------------------------- 21 Tilting and breaking the rocks ------------------------------- 29 Isle Royale-a small piece of the big puzzle ------------------ 34 What happened when? -------------------------------------- 35 Time as a geologic concept --------------------------------- 36 What was there before-the pre-Keweenawan -------------- 37 The rocks of Isle Royale-the Keweenawan ----------------- 38 The missing chapters --------------------------------------- 40 The glaciers take over -------------------------------------- 41 Glacial effects on the land ---------------------------------- 41 Glacial effects on lake levels -------------------------------- 47 Some minerals of special interest ---------------------------- -
New Mexico Bureau of Geology and Mineral Resources Rockhound Guide
New Mexico Bureau of Geology and Mineral Resources Socorro, New Mexico Information: 505-835-5420 Publications: 505-83-5490 FAX: 505-835-6333 A Division of New Mexico Institute of Mining and Technology Dear “Rockhound” Thank you for your interest in mineral collecting in New Mexico. The New Mexico Bureau of Geology and Mineral Resources has put together this packet of material (we call it our “Rockhound Guide”) that we hope will be useful to you. This information is designed to direct people to localities where they may collect specimens and also to give them some brief information about the area. These sites have been chosen because they may be reached by passenger car. We hope the information included here will lead to many enjoyable hours of collecting minerals in the “Land of Enchantment.” Enjoy your excursion, but please follow these basic rules: Take only what you need for your own collection, leave what you can’t use. Keep New Mexico beautiful. If you pack it in, pack it out. Respect the rights of landowners and lessees. Make sure you have permission to collect on private land, including mines. Be extremely careful around old mines, especially mine shafts. Respect the desert climate. Carry plenty of water for yourself and your vehicle. Be aware of flash-flooding hazards. The New Mexico Bureau of Geology and Mineral Resources has a whole series of publications to assist in the exploration for mineral resources in New Mexico. These publications are reasonably priced at about the cost of printing. New Mexico State Bureau of Geology and Mineral Resources Bulletin 87, “Mineral and Water Resources of New Mexico,” describes the important mineral deposits of all types, as presently known in the state.