Website http://www.wcgmc.org/

Two pleurodictyum coral and and a brachiopod from Indian Yellow Night for WCGMC (see pg. 2) It is Party Time! Creek (see page 6)

Club Workshop, Saturday, Dec. 12th WCGMC Christmas Party is HERE Bring your rocks to saw and polish. The workshop is 6:00 PM, December 11th open to all paid club members; we do ask for $5/visit Presbyterian Church, Maple Court, Newark, NY from each adult to help maintain equipment. We plan to hold similar workshops once a month through the If you did not sign up while at the November winter months. meeting, please let us know. A call or note to either Eva Jane Weiler, Linda Schmidtgall, or When: 10:00 AM til mid afternoon, Sat. Dec 12th Fred Haynes will do the trick. We need to Where: The Weiler’s Barn and Workshop have a head count to insure we have enough 6676 E. Port Bay Rd, Wolcott, NY meat, potatoes, and gifts! Rules: BYOR (Bring your own rocks) to saw, grind, polish or even facet. Training on equipment After signing up, it is very simple: is available. Eye protection is recommended.  Note the earlier start time of 6:00 PM  Club will provide meat, potatoes, drinks  Bring a dish to pass (dessert or entrée)  Club will have a mineral gift for all and Linda is busy concocting a fun and new way for you to “earn” it.

December, 2015 Wayne County Gem and Mineral Club News p. 2

Yellow Mineral Sunshine volcanic gases and native can form in vugs and along Yellow is the color of sunshine, of fractures in volcanic rocks, but the brilliant warm summer days. It is best sulfur crystals form when the color of bananas, lemon sedimentary gypsum deposits are meringue pie and butter pecan ice reduced (oxygen stripped for cream. There are beautiful yellow sulfate). breasted birds and wondrous yellow flowers. Some cultures view yellow as the color of happiness, amusement, and even optimism.

All that is well and good, but You can spot the sulfur in the upper left yellow is also the color of and probably the honey colored dogtooth calcite in the middle of Stephen Meyer’s wulfenite, sulfur, heliodor and a display, but can you see the ? number of other wondrous Here let me help you out! and gems. And, of Linda had more than sulfur to display. course, it is the color of gold. It Travertine from Ilion may not be classic yellow, but it counts, and it is pretty.. was with this appreciation of the color yellow that WCGMC In Arizona, PbMoO4 is love! And convened in November for a sometimes this love is yellow. celebration of “Yellow Minerals”. The square thin transparent crystals are also quite fragile. The quintessential yellow mineral This secondary mineral in - is undoubtedly native sulfur. The rich ore deposits requires an arid simple native element mineral is environment to form and be Of course, there were other yellow the definition of yellow, no color preserved. Morocco and Mexico metallic minerals on display. modifier is needed. are other locations where colorful Chalcopyrite and pyrite are often wulfenite can be found, but the referred to as fool’s gold, but they mineral was discovered, and remain collector favorites. Pyrite named, after a location in is cubic and chalcopyrite is Slovenia in eastern Europe. tetragonal and both show off these forms superbly.

Linda Schmidtgall’s sulfur was the largest and brightest of several that were brought to the event.

Sulfur is a common element in the earth’s crust, but it is usually combined with oxygen in minerals like gypsum or with metal elements in minerals like pyrite. Four of the five wulfenite specimens I Two inch chalcopyrite specimen from Sulfur is a common element in brought to “the show” were self collected China. in Arizona. December, 2015 Wayne County Gem and Mineral Club News p. 3

when exposed to long wave ultraviolet light.

Ed Smith had a nice pyrite specimen, but he also brought a number of faceted citrine crystals. Gary Thomas collects fossils and he was not going to be left out. I think In addition to gemstones like this specimen has been doctored a bit citrine and heliodor, there is a lot though. of lapidary material that comes in Generally we do not think of shades of yellow and orange. fossils when we think of the The club has a bit of Carnelian color yellow. There are, agate which tends to best display however, yellow pyritized its brilliance once cut. fossils. We collect them at Bill Chapman brought this drab massive block of scapolite (Var. wernerite) to the event. You Alden every year, and several had to go into the back room with his black were on display from Club light to see its special color. members.

Carnelian agates.

Some minerals don’t show off their spectacular yellow colors without a little help. Scapolite But, this excellent pyritized comes to mind. Typically a drab ammonite is not from Alden and it grey, bluish grey to beige mineral is not Devonian. It is not even when found in the metamorphic from North America. Stephen rocks of the Adirondacks, most Mayer displayed this Pleuroceras sp, which is from the Early scapolite lights up canary yellow Jurassic of Germany. ======

December, 2015 Wayne County Gem and Mineral Club News p. 4

A Test of your Dinosaur Knowledge

November Workshop News – Another Sphere Machine

Here are postage stamps issued by Romania, Montserrat, and Antigua & Barbuda. They are part of sets of dinosaur stamps issued by the respective countries. Each contains an egregious paleontology error. Can you find the mistake in each stamp? Turn to page 7 for the answers.

A week in the Carolina Mts.

Have you ever considered attending the Eastern Federation of Mineralogy and Lapidary Society (EFMLS) Wildacres workshop in North Carolina? Now is the time to think about the pair of week long 2016 opportunities (May 9-15 and September 5-11) for learning and camaraderie with others who share our passion for the hobby.

Take classes, listen to expert speakers,

A. Our president has built yet another sphere machine. This join a field trip, and otherwise enjoy a peaceful week of lapidary fun at a one is for really large orbs. B. The Ilion travertine continues to fantastic retreat just off the Blue Ridge yield some stunning polished slabs. This one is 3” across. C. Parkway. Partially funded, the event will The “old” sphere machine was in action with a piece of rose only cost you $400/person for full room quartz. D. Glenn explains to Bill how his new machine works. and board. He is demonstrating how large a sphere he can make with his hands. We are all waiting to see the first Jupiter sphere. For details visit the EFMLS Wildacres website.

December, 2015 Wayne County Gem and Mineral Club News p. 5

World’s Largest acquisition efforts fail we can display these stamps instead. It happened last month in

Botswana, a land locked country in southern Africa. While processing kimberlite rock for , the Lucara Diamond Corp. struck gold, well not literally. The Karowe kimberite pipe was What they unearthed was the discovered in 1969, but was not further largest gem quality diamond pursued until 2000 when drilling indicated the volcanic pipe of diamond-bearing found in more than 100 years kimberlite was comprised of three lobes anywhere in the world. and was considerably larger than Botswana has issued a number of stamps previously estimated. commemorating its diamond industry.

Included is a set in 2001 where the stamp Finally, in 2008 Botswana issued itself is shaped as a cut stone. a development license to Lucara Diamond Corp., a Canadian How do Diamonds Form? company headquartered in Vancouver. The first diamond Diamonds require extremely high was extracted in 2011 and mining temperature and pressure, and has proceeded at a rapid pace significant time to form. For this since. Lucara reports a reason most of the earth’s diamonds production rate of about 400,000 grow 140-170 kilometers (over 90 miles) beneath stable continental carats/year. At that rate this regions. Temperatures of greater single diamond represents about than 2000ºF are also required. Is it real? This may look like a misformed one day’s worth of production. garden variety ice cube or maybe a piece But formation is not enough for us to of quartz from a pegmatite, but it is not. It Lucara has not yet decided when enjoy their brilliance as no one has is a 1,111 carat diamond discovered on or how to sell the stone, and it is November 16th, 2015 at the Karowe Mine figured out a way to access the rock in central Botswana. Measuring 65mm x not clear whether it is of more at those depths. Magmatic 56mm x 40mm, the cabinet size mineral value uncut or fully faceted. processes capable of carrying specimen is purported to be the second Interestingly, the stone is too large fragments of the mantle rock from largest gem diamond ever recovered. for Lucara’s onsite scanner so it those depths to the surface are also will very likely need to go to required. Such volcanic events It was actually fortuitous that this Antwerp, Belgium to be properly (called kimberlite eruptions) are rare diamond was recovered whole. accessed for cutting to maximize even in geologic time and none have Kimberlite rock below the upper occurred since man has been around value from the stone. 10m of weathered surface is hard to observe geologic processes. and it is routinely crushed to permit recovery of diamonds via density separation and hand screening. Had this diamond undergone such treatment a whole lot of smaller diamonds Despite this uncertainty stock in the small would have been recovered Canadian mining company jumped 32% instead of this behemoth. when the find was first announced on Nov. 19th. However, the rock containing this diamond was subjected to WCGMC is investigating the screening by a new type of X-ray feasibility of purchasing this stone. technology called XRT sorting, If we are successful we will which can measure the atomic display the uncut gem next density regardless of surface June at GEMFEST in interference. Translation: the Canandaigua. Subsequent to that dense mineral could be it would be our plan to facet the detected inside the rock and stone in our club workshop. If our Kimberlites carry diamonds from saved from the crusher. their source at 140-170 kilometers. December, 2015 Wayne County Gem and Mineral Club News p. 6

There are many well known fossil Furthermore Gordon Baird (pers. fossil bed. Multiple species of collecting sites in the creeks and comm.) recalled a repeated brachiopods including gullies draining into the Finger Menteth unit somewhere up Spinocyrtia granulosa, Lakes (places like Kashong Indian Creek. Mucrospirifer mucronatus, Gully, Deep Run, and Portland Rhipidomella sp., and the Point to name a few). But for ubiquitous Tropidoleptus every well documented site there carinatus were waiting to be are a dozen lesser known locales collected, but my day was made where drainages into the Finger finding three perfectly symmetric Lakes expose the fossil rich and complete Pleurodictyum strata of the 385 million year old americanum. You may recall Middle Devonian Hamilton from an earlier newsletter that Group. Indian Creek, near “pleuros” are my favorite fossil Williard on the eastern side of Indian Creek in the fall: Can you spot and this was a new locality for Seneca Lake, is one such Stephen Mayer in perfect paleontology me to boot. posture? location. Even armed with all this Upon entering Indian creek off of wonderful input, Stephen and I East Lake Road just north of the could not convince ourselves that hamlet of Willard, one we were not in a straight forward immediately encounters a unit Kashong shale section as we with large irregular concretions waded upstream. Perhaps it was exposed in the bedrock. To an all the fallen leaves that covered untrained eye some might even the pertinent geology, but more be confused with dinosaur than likely our failure was that we bones. One land owner that had our eyes glued to the shales Stephen Mayer and I visited looking for fossils. While we did during an October excursion was not get leave with a comfortable absolutely convinced of this and A Pleurodictyum americanum as understanding of the stratigraphy encountered in the creek bed. Note the had even built a nice wooden we did leave with some fossils. Tropidoleptus in the lower middle. They stand to hold his prize “bone”. were truly everywhere.

Given that the Menteth limestone is exposed at the lakefront in this region, one would suspect that these concretions and the entire stratigraphic section in Indian Creek would expose the overlying Kashong and Windom Pleurodictyum americanum are tabulate Shale members of the Moscow corals noted for their polygonal corallites. The three I found in the Formation. However, it is not Kashong shale of Indian Creek are also that simple. There is apparently symmetric in overall shape. some faulting in the area which Traversing the Kashong shale, we may lead to repeat section in the found a few trilobite pieces, here a Another interesting aspect of creek bed. Jacobi (2002) pygidium, and lots of Tropidoleptus Pleurodictyum coral is that they brachiopods like the one hiding behind appear to require a hard mapped major cross-faults in the George Washington’s head. creek and Luther’s 1907 Seneca substrate on which to grow. Lake bedrock geology map About 1500’ from Lake Road and Some grow on rocks, others on shows older rock than Menteth at a major fork in the creek we carbonate hardgrounds, but the extending up Indian Creek. encountered our first bona fide December, 2015 Wayne County Gem and Mineral Club News p. 7 most common substrate seems walk up each to find ourselves References: to be another fossil (Brett and stratigraphically. Perhaps we can Brett, C. E. and Cottrell, J. F., 1982, Cottrell, 1982). find the phosphatic pebble bed at Substrate specificity in the Devonian the top of the Kashong member tabulate coral Pleurodictyum, near the base of the Windom. Lethais, V. 15, p. 247-262 Moreover, maybe we will Haynes, F. M., 2014, Pleurodictyum traverse the entire Windom and americanum, WCGMC News, Nov. find the Tully limestone that caps 2014, p 2-3. the Moscow Formation. This could establish where we were Jacobi, R.D., 2002, Basement Faults collecting. Until then, knowing and seismicity in the Appalachian that we were in the Kashong Basin of New York State, Tectonophysics, V. 53, p. 75-113. I guess with all the Tropidoleptus shale member will have to brachiopods around, it should not be suffice. surprising to see one of the Luther, D.D., 1907, Geology of the Pleurodictyum I found growing on the Geneva-Ovid Quadrangles, NYSM common brachiopod of the time. Can Bulletin 128. you see it on the base of the coral? Meanwhile the Tropidoleptus are literally a dime a dozen. Indian Creek does not appear to be

posted, but as with all creeks and off Indian Creek splits into two major road regions along the Finger Lakes creeks about 1500’ from the lake. permission to enter should be We walked each fork a short sought before entering. distance, but had spent our And last but certainly not least, I believe energy for the day collecting this brachiopod is an Orthospirifer fossils near the confluence. We marcyi. Regardless of genus, it is a fine pedicle valve specimen from a new will need to return next year and locality.

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December, 2015 Wayne County Gem and Mineral Club News p. 8

Wayne County Gem & Mineral Contacts Bill Chapman – Field Trip Chair Glenn Weiler – President [email protected] [email protected] 607- 315-594-8478 868-4649 Jerry Donahue – VP [email protected] Fred Haynes – Newsletter Editor 585-548-3200 [email protected] 585-203- Eva Jane Weiler – Secretary [email protected] 1733

315-594-8478 nd Bill Lesniak – Treasurer/Webmaster Club meets 2 Friday of each month starting in [email protected] 315-483-8061 Sept. Board of Directors Mini-miner meeting at 6:30 PM. Ken Rowe [email protected] 315-331-1438 Regular meeting at 7:00 PM Susie Hoch [email protected] Park Presbyterian Church, Maple Court, Newark, 585-794-7287 NY Linda Schmidtgall [email protected] 315-365-2448 Website – http://www.wcgmc.org/ Laurie Frey [email protected] 315-483-9894 Dues are only $15 individual or $20 family for a full season of fun. Send to WCGMC, P. O. Box 4, Newark, NY 14513