From: "Gary Grenier" <ggrenier@erols.com> Date: Sat, 11 Jul 1998 13:24:56 -0400 From: Gary Grenier <ggrenier@erols.com> To: "Earl Verbeek" <ILMNVC65.ILMNVD65.everbeek@nv.blm.gov>, "Earl Verbeek" <everbeek@nv.blm.gov>, "Gary Grenier" <GGrenier@iqcity.com>, "George Elling" <George_Elling@usccmail.lehman.com>, "Jay Linninger" <matrix@redrose.net>, "Jim Chenard" <JimChenard@compuserve.com>, "John Jaszczak" <jaszczak@mtu.edu>, "Mark Leger" <MRAGATES@aol.com>, "Peter Chin" <Peter.Chin@uspto.gov>, <rbostwick@spexcsp.com>, "Steve Misiur" <zincer@CERF.NET>, <UVSYSTEMS@aol.com>, "William C. Mattison" <mattison@apwk01g1.nws.noaa.gov> Subject: FrOg #4 News and Chat Group Issue Welcome to the FrOg #4 (Franklin-Ogdensburg) News and Chat Group ------------------------------------------------------------------------ As previously mentioned, I am the facilitator who gathers, extracts, and sends your reformatted text or what ever I gather that may be of interest along to Dan Russell. He then paginates and rebroadcasts the text to our group. Unfortunately, Dan Russell has lost his personal IP account and thus e-mail has been suspended while he locates another. I on the other hand, will be changing IP services providers and e-mail addresses by July 15th. An e-mail with new addresses will be snet to all, so please bear with us through the transition. Al lot is going on in and around the world of mineralogy. This time I will present a variety of topics, new web page addresses, and extracted e-mails form outside the group. I will present many of these topics in the hope that I encourage your participation and sharing of information to the group. ------------------------------------------------------------------------ Subject: Sterling Hill Swap-n-Sell, May 2-3, 1998 The event was a big success with fair weather after threatening skies. The dealers arrived early and customers were sporadic on Saturday. Reports of Sunday activity indicated a much better turnout. The 3rd annual auction was held in the Ogdensburg Fire House meeting room. Everyone who attended was treated to a dinner and fine comradeship. Many fine specimens were sold from three collections that had fine old labels from important old collections including the Bement and US National Collections. The species offered included two ganophyllites, a bannisterite, a roeblingite, willemites, franklinites, andradites, tephroites, yeatmanites, kolicites, rhodonites, manganaxinites and many others. All and all the auction sold approximately 130 specimens and raised over $12,000 for the museum. During the Sterling Hill outdoor swap I was able to observe some of the rare species as follows: Hydrotalcite: Report of observed specimen from Steve Kuitems Collection Hydrotalcite appears as 3mm yellowish cream to brown stained hexagonal platy crystals with vitreous to glassy faces. The crystals appear on edge as folio pages and penetrating growths clumped in cavities and vugs in a seam with orange-yellow platy 2mm spherical crystal clusters of hauckite. Also in the seam and associated with the hauckite and hydrotalcite are gemmy red masses and small hemimorphic zincite crystals. The matrix is composed of white calcite with sparse granular masses of willemite. The vugs and cavities are small to .75" and are in the narrow seam that is cutting midway through the matrix. The contents of the vugs and cavities are easily overlooked. Franklin specimen. Descloizite: Report of observed specimen from Steve Kuitems Collection The descloizite formed very small yellowish-orange cubic-like single crystals to .5mm dispersed on an altered dark brown "Jeffersonite". On the edge of the specimen in a small cavity can be seen a thin crust form cluster of descloizite crystals. From the Edwards collection - Sterling Hill Synadelphite: Report of observed specimen from Steve Philips Collection What initially caught my eye was the dark brown stain on the corner of the kraisslite face. Upon closer inspection with a hand lens the synadelphite appears as tiny dark brown stained prismatic radiating crystals on the kraisslite. The kraisslite is bronzy and fine-grained appearing as a seam filling in granular red willemite, franklinite ore from Sterling Hill. The synadelphite appeared to be on and in the kraisslite not having direct contact with the red willemite ore. The synadelphite appeared to be undamaged and sharply terminated with vitreous crystal faces. The crystal form is distinctively different from the eveite which forms flattened honey yellow to tan-brown lath-like lattice works of crystals on kraisslite with chlorophoenicite. There is no apparent chlorophoenicite on the synadelphite bearing kraisslite. Sterling Hill specimen. ------------------------------------------------------------------------ Subject: The Picking Table is Getting Back on Schedule Reports from Dick Bostwick have the Spring-98 issue at the printer and soon to be in your mailboxes. When this issue is delivered the Picking Table will be formally back on schedule with the next issue coming out in the fall. Dick hopes that the mailing of the fall issue will coincide with the fall FOMS mineral show that is in late September. Quick note, by now you should have received your "Spring '98" issue of the PT. Congratulations to Bostwick for putting the PT back on schedule! The fall-98 issue is going to make history. For the first time color images are going to be published in The Picking Table. Since this is going to cost more than the usual publishing expense for the PT a "Color Fund" has been setup to receive donations rather than raise dues. Please consider offering a donation to the club for this worthy effort. ------------------------------------------------------------------------ Subject: Rocks & Minerals Magazine Does a Story on Sterling Hill Latest Issue of Rocks & Minerals Magazine has a color story about the "Hill". While briefly describing all of the many features of the Sterling Hill tour and facilities, the story presented collector notes from past field trips into the Passaic and Noble pits that should inspire other more distant collectors to become active. The R & M did Sterling Hill a good PR service. Pick up an issue, you won't be disappointed, and it might just become a collectible? ------------------------------------------------------------------------ Subject: FrOg E-mail Date: April 20, 1998 From: Bill Mattison "William C. Mattison" <mattison@APWK01G1.nws.noaa.gov> Hi Gary, A thought concerning the FrOg on-line occurred to me over the weekend. I don't recall the full list of who gets the FrOg news e-mails, but what I do recall is that most everyone on the list is an advanced FrOg collector. I would expect questions to be very few and far between. Suggestion: have Doug Mitchell tell the FMS online about the FrOg news group, and see if that gets you a bigger audience with more less-advanced collectors. Then you'll get more questions. Also, notice also how sporadic FMS online is. It goes through busy spells; it goes through quiet spells. It's natural that FrOg online will do likewise. I do have a couple more things for FrOg online, but I'm waiting for FrOg #3 to come out first. I find more shorter messages is better than fewer longer messages. Things get missed with the longer messages. Since I did not get FrOg #2 until you sent it to me separately earlier this month, check with me when FrOg #3 goes out to make sure I receive it. By the way, did anyone else receive FrOg #2? I saw Dick Bostwick this past Friday; it seems he did not get FrOg #2. Bill: I have sent out a copy of FrOg #3 which you should have received before this. I am now curious as to who else may not be receiving the FrOg. If anyone has received a FrOg, then you are still on the mailing list (unless you asked to be removed), so let me know if you are not getting the e-mail. Also, I will be checking with Dan to get the current roster of e-mail addresses. Sometimes the addresses change and we do not get the change, so let me know. Gary ------------------------------------------------------------------------ Subject: Fluorescent Mineral Identification Date: June 5, 1998 From: Bill Mattison "William C. Mattison" <mattison@APWK01G1.nws.noaa.gov> Hi Gary, I have a question for the group. I have a couple of specimens, smallish, with a little Margarosanite, some Clinohedrite, some very tiny specks of red fluorescence (Calcite, probably), Willemite, and lots of something that fluoresces Hardystonite blue. I can think of three minerals this blue fluorescing mineral could be: Hardystonite, Prehnite, or Xonotlite. Claude Poli would say it's "pecto-prehnite", a mix of Pectolite and Prehnite. * Well, the fluorescence doesn't seem "electric" enough to be Xonotlite, and it's massive, not a coating or crack filling. But then, I've seen so little Xonotlite in my life, I can't say I know the range of fluorescence colors Xonotlite fluoresces. * The assemblage seems wrong for Hardystonite (well, at least IIIIIIII've never seen or heard of Hardystonite and Margarosanite occurring together, but then this i-s Franklin!). * "Pecto-prehnite"? Apart from Claude, I've never seen or heard of that either. Do these mix at such a scale that even with about 3x magnification it looks like one solid mineral? Ok, ok, this is Franklin! * Prehnite's fluorescence does cover a range of colors. Is Hardystonite blue in that range? The only analytical techniques practically available to me at this time are fluorescence, association, and white-light color. The Hardystonite blue fluorescence is under SW, the mineral is dead under MW, and under LW is mostly dead but shows some weak Bustamite-like red-violet fluorescence in a few areas. I'm at work and the rocks are home, and I don't recall this mineral's white-light appearance, but I do recall seeing no hint of Bustamite. What is this mystery mineral? How can I determine what I've got? Bill: As far as your question about fluorescent species distinguishment, I am sure that members of FrOg can help. So, I will give it a try and then ask the group to respond as well. With respect to the pale blue FL responses in the margarosanite - clinohedrite specimen, there is not enough specimen information to provide you with an accurate species label. However, from what I have seen in other collections, margarosanite mixes freely in celsian and hyalophane rich matrixes. If the margarosanite is disseminated throughout the matrix it could be very hard to identify. The best way to be sure is to have Dick Bostwick to a look or send a fragment off to Excalibur for analysis. As far as the xonotlite FL response is concerned, I have never had any difficulty distinguishing the intense violet-blue response from others. In addition, xonotlite is far less plentiful and far more restricted in the assemblages in which it is found than other blue to violet fluorescing species. Xonotlite is more often seen in tight bunches of white to cream colored acicular xls in jack-straw to radial masses forming last as a reaction product of weathering matrixes often composed of hancockite, datolite, clinohedrite, willemite, thomsonite. Also seen in massive prehnite (which is white to gray and somewhat platy) with masses of pectolite (which is white and often glassy) in better specimens. In others, these two species form a "soup" of small grains cemented together to form and almost indistinguishable mass that is broken up by the occasional andradite or franklinite grains mass. Often at the contact of the pectolite/prehnite grains with the andradite or franklinite there will have formed a reaction rim of pale blue-white fluorescing margarosanite. In the past this has been misidentified as prehnite. It is possible that prehnite has a pale blue-white response, but I know for certain that prehnite has peach-pink SW response. It is important to remember that prehnite mixes often with other species that fluoresce which makes identification confusing and most difficult to distinguish the individual grains. Check PJD's latest 5-vol work for helpful daylight detection help. Gary If anyone else want s to take a stab at FL identification, please do. ------------------------------------------------------------------------ A New Web Site for All Mineral Enthusiasts The MINERALIST http://www.flash.net/~summit1/mineralist/mineralist.htm MINERALIST Welcome to the "Mineralist" Information Page. "Mineralist" is a moderated email list service intended to facilitate relatively noise-free discussions of issues in and about specimen mineralogy and related geology topics. Bookmark this page for easy referencing of the "Mineralist" documents and "Mineralist" archive. Mineralist was launched on March 24, 1998. Mineralist Documents Mineralist Charter Mineralist Subscription Information Mineralist Posting Guidelines Mineralist Moderation Guidelines Mineralist Frequently Asked Questions (FAQ) Mineralist Archives I discovered the above copy of the web page during one of my random searches through the internet. It has proven to be very interesting on a global mineralogy basis. Perhaps you will find it interesting as well. Gary ------------------------------------------------------------------------ Interesting E-mail from Mineralist In an effort to introduce this next topic I must add that a common conversation topic among Franklin and Sterling Hill collectors is that of mineral identification services; where are they, what do they do, how much do they cost, and how quickly can analysis results be provided. MINERAL ANALYSIS Mineralist <minlist@flash.net> Alfredo Petrov Writes: A question for the mineralogists or chemists among us: Being a geologist and mineral collector in a country with no professional mineralogists, I find myself frequently sending off specimens of "whatzites" (to borrow Mark Bandy's term) to mineralogists in Europe or the USA for identification. The replies I get back refer to analyses being done by various procedures, like microprobe, EDX, X-ray fluorescence, Raman or Mossbauer spectroscopy... (Or I hear that something can't be done because one or other of the above instruments are broken :-( It would be helpful for us amateurs if one of the professional chemists or mineralogists on the List could explain what the differences in these methods are; i.e. differences in their capabilities, accuracy's, sample size needed, elements detected, etc. I know some methods don't detect very light elements; most can't distinguish Fe2+ from Fe3+; some need much larger sample sizes from others; etc. I think having more knowledge about these techniques would help us not to inundate the overworked professional mineralogists with inappropriate samples. Thank you. Alfredo Petrov, Cochabamba, Bolivia fred@bo.net Gail Dunning Writes: For those of you out there who rely on others to perform analytical identifications of mineral specimens, it is not easy to determine which analytical technique is best for a specific mineral in question. I do both in that I do certain mineral identification but also I send specimens out for identification. There are several analytical techniques out there which will aid the mineral collector to properly identify his (or her) samples. For myself, I only have the capability to perform EDS (Energy Dispersive Spectrometry) using the SEM with BSE (Backscattered electron imaging) First, EDS has certain limitations. With a light element detector, one can see with fairly good reliability oxygen, if elements with high atomic number are not present in high percentages (these elements absorb the weaker X-rays of the lighter elements). Sample size can be small, about 0.1 mm in size usually is sufficient if pure. For my specimen identification I always do EDS first to determine what elements I am dealing with, then based on what I see, I make a decision what to do next. I use a search program to reduce to a reasonable size what possible minerals I have using any physical properties I can gleam from the specimen. If this does not work, then I send the specimen for X-ray diffraction, which generally is the final "nail in the coffin" for identification. I have found that a combination of EDS and powder diffraction is the fastest way to identify minerals. There are certain limitations to EDS analysis (it only sees element levels about 1% or larger without element interference). Some element spectrum lines hide behind the lines of other heavier elements, which can cause problems, such as S behind Pb and Ti behind Ba. There are other examples of interference. The bottom line in EDS mineral identification is to have a reliable standard of known minerals to use as a comparison. I have used this technique for many years and it works fine. Whenever I obtain a mineral, which has been verified by X-ray diffraction, it becomes an EDS standard. EDS is also good for the opaque minerals such as sulfides, sulfosalts, etc. These minerals are first made into a polished section and then examined in the SEM using BSE which can distinguish atomic number differences if more than one phase is present. SEM/BSE/EDS combined with optical microscopy is a powerful set of identification tools. In certain cases microprobe must be used to obtain analytical composition of the opaque minerals, especially when a specimen can have several intergrown phases, such as the sulfosalts. The probe is great but hard to find a willing investigator with time. The availability of mineral identification people has been reduced in the past years due to budget cuts and other priorities. To show what the SEM/EDS can do, our mineral collecting group has identified nine new minerals, which are currently being studied by others. It does work, but it takes experience. Gail Dunning Gary Grenier Writes: Alfredo: I cannot agree more with your observation regarding a general lack of information and understanding regarding mineral quantitative, qualitative, and microprobe analysis. It would be very useful to have more information, however even more important to the mineral collector is having a list of analysis service providers. For instance, Excalibur Minerals provides analysis services for a fee. Are there any others? Gary Grenier [ggrenier@erols.com] Laurel, MD Don Newsome Writes: Gary, There is another one that provides analysis services he is Bart Cannon, he runs Cannon Microprobe and lives in the Seattle, WA area somewhere. Don Newsome Renton, WA uvsystems@aol.com http://www.globalpac.com/gems/uvsystems Henry Barwood wrote: It would be helpful for us amateurs if one of the professional chemists or mineralogists on the List could explain what the differences in these methods are (EDS, XRD, XRF, SEM, TEM, etc.); i.e. differences in their capabilities, accuracy's, sample size needed, elements detected, etc. Can't speak for the majority, but when presented with an unknown I normally proceed in a certain order: 1) Visual examination to determine any easily observable clues such as morphology, luster, specific gravity, streak, cleavage. This eliminates most common things and points to what should be done next. 2) If there is sufficient sample an XRD using a diffractometer is in order to try and identify the mineral, or if the specimen is a mixture of minerals. If only a small amount of sample exists, a powder diffraction camera photograph is prepared and analyzed. 3) At this point we usually have either a) a known species bases on XRD, or b) an unknown species or mixture. If the species is one that has isomorphous substitution, then a chemical analysis is in order. If it is an unknown, a chemical analysis is a necessity. 4) For a quick qualitative, or semi-quantitative, analysis an EDS spectrometer mounted on an SEM is usually the instrument of choice. There are two pitfalls that should be noted with this method: a) the EDS analysis is a SURFACE analysis and is subject to mis-interpretation (I have specimens of goyazite with a thin skin of svanbergite, for example) b) the peaks displayed are difficult to interpret and the difference between 1-2% Fe and 10-20% Fe can be rather subtle depending on the matrix (1-2% Fe in variscite seems quite large, but 10-20% Fe in ilmenite/pyrophanite can seem insignificant). 5) For a complete analysis the microprobe (WDS spectrometer) is preferred. Even here calibration and dehydration errors are common. A skilled operator and experience are helpful. 6) If the mineral is a true unknown, then tests for Fe++/Fe+++, LOI, optics, etc. are needed. The best weapon is careful observation and learning some simple physical, chemical and optical tests. Henry Barwood Subject: Analytical tools Date: Sun, 31 May 1998 11:20:21 From: Mineralist <minlist@flash.net> Pete Richards Writes: I'd like to amplify what Henry Barwood said about the importance of simple tests. I am painfully aware that when collecting rare species or places with complex mineral assemblages, these may be insufficient, but I suspect that many collectors could at least narrow the range of possibilities, and often make positive identification of specimens which are either unidentified or sent to specialists who do, after all, have something else to do... >:^) Most mineralogical texts from the '60s and before have substantial sections on determinative mineralogy. Optical tests are very powerful, but somewhat out of reach of most, since they require a petrographic microscope and various other equipment which is not easy to learn to use well, but also expensive even used. However, simple qualitative chemical tests such as blowpipe tests and bead tests (using molten borax or sodium carbonate or similar chemicals to dissolve fragments of the mineral) do not require fancy equipment and, once you learn to use them by practicing with known minerals, can tell you a lot about an unknown. A simple example: at a recent trip to Mont. Saint-Hillarie, someone gave me a piece of breccia which contained green andradite (not uncommon there and recognizable by color and morphology), brown vesuvianite or tourmaline, and gray molybdenite or graphite. I determined that the brown mineral was vesuvianite by melting a fragment with a butane microtorch and watching it bubble as it melted quite easily. This fits nicely with the description of vesuvianite as fusible at 3 (i.e. rather easily) with intumescence, but not with the tourmalines, most varieties of which are infusible or only fusible on very thin edges. The gray mineral was, as suspected, molybdenite, based on the fact that it was soluble in nitric acid. I could have tested with some other reagents, which yield a colored solution when molybdenum was present, but I did not feel it was necessary in this case. I could have done a streak test, but I find it hard to be sure of the difference in streak color between moly and graphite. At any rate, with a little reading in the textbooks to choose my tests and less than an hour of fooling around in the basement, I identified these two minerals to my satisfaction. Admittedly, if the brown mineral did not look like anything familiar, or if it could have been any of 8 different species, I would have preferred the greater certainty of x-ray/EDS approaches. Pete Richards Harry Barwood Wrote: I would like to amplify somewhat Pete's excellent advice. Here are some inexpensive techniques I have seen applied by amateur mineralogists with great success: 1) Simple chemical tests. This can range from bead tests to fairly complex microchemical tests. Curt Segeler used to teach the ring oven technique to Scout classes. When Curt would send me something to identify it usually had a note like "... I tested this and found selenium and copper but no lead. It was identified as demesmaekerite... Can you help me out with this one?". 2) Optical tests. These can range from a simple R.I. determination using even a rudimentary (non-petrographic) microscope to sophisticated tests such as using the spindle stage. A late friend taught himself petrography and used the spindle stage with such accuracy that most of my identifications for him were simply confirmation of his identification. Even very inexpensive microscopes can be converted to use polarized light and R.I. oils are not excessively expensive (they can even be made at home with a bit of skill). [Mod. Note - "R.I." means "refractive index", referring to the degree to which incident light is bent or refracted upon entering the substance] 3) Physical properties. Never underestimate the value of streak, luster, specific gravity, hardness and cleavage in separating minerals. Small grains and fragments can be tested for S.G. with excellent accuracy and a set of hardness points is invaluable. An excellent example! I would like to use a quote from the late Neal Yedlin: "Buy and use a good book!". In this case a good elementary mineralogy text. Henry Barwood ------------------------------------------------------------------------ NEW Topic: DIGITAL CAMERAS AND MINERAL PHOTOGRAPHY I have been studying digital cameras for possible use in mineral studio and field photography. My objectives have been very simple. I need a camera that will duplicate the close-up results that I am able to get with my Pentax 35mm SLR with a Macro lens. In searching and trying the many digital cameras on the market I have had to develop a new photographic vocabulary as well as appreciate the need for more computer equipment. The following e-mails and extracted adds from the internet reflect on the growing availability and complexity of the digital camera solution. I encourage any and all who are interested in adapting the digital camera or video-cam mineral photography and image re-presentation share their findings with the group. My first search for information led me to (2) magazine publications; Camcorder and PC Photo. Both of these magazines publish camera reviews. Based on what I have read in these magazines I visited web sites looking for more detailed information. For the most part this leads to information overload, so live trials are a necessity. I tried both of the Sony Mavica cameras 5 & 7. The Sony Mavica has the benefit of using a floppy to transfer images to your computer. It also records at a 640x480-pixel image size. The camera can be set to low resolution as well as high resolution. I have included a sample image as an attachment for you to view. I found the Mavica easy to use and reasonable in cost at $599.00. In testing the close-up ability of the camera I found that the viewfinder and the actual recorded image were not synchronized. It was easy to move to close to the subject and shoot an out of focus image. Even though the camera has a playback screen, the photographer can not detect the out-of-focus nature of the image until it is on the computer monitor. The average range of a close-up image can be determined by how close the camera can be moved to the subject mineral, in the case of the Mavica by trial and error. I found the Mavica to allow a camera to specimen distance of 9" to 12". I tested similar fixed lens through the viewfinder cameras that include the Olympus D300L, the Ricoh RDZ-300z, and Cannon Powershot 350. In all cases the pixel image size was critical to the quality of the resulting image. The Olympus D300L is better at 1024x768 as is the Ricoh and Cannon. The better cameras will shoot a 1560x1280-pixel image size or better. The big drawbacks with any and all of these cameras are that they have a fixed lens not through the lens image finder with a fixed focus range. In asking mineral dealers on the web what they use I found the following: Subject: Digital Cameras Date: Monday, 9 Feb 1998 21:30:14 -0500 From: OsoSoft Mineral Connection http://www.osomin.com Greetings, I use a video camera designed for video conferencing, along with a Snappy video capture device on The OsoSoft Mineral Connection. Since the Snappy has a video passthrough, I use a 13" color TV as a monitor for focusing, etc. The camera cost just $89 from Damark, and the Snappy sells for about $150 street price. The TV was surplus at my house, so cost nothing. This system works OK and is very fast to use, which is critical for me since I have to take dozens of photos in a session to post items for sale on the site. It's not as high quality as shooting on film, then having the images put on disk, of course, but you don't have to wait. The biggest advantage of the video system is that the camera focuses as close as necessary, even to the front element of the lens, making it easy to shoot thumbnails, etc. Also, I've adapted it to my stereo microscope for use in photographing micromount specimens. You can see that setup explained on the site. Best wishes, George Campbell OsoSoft Mineral Connection http://www.osomin.com Subject: Digital Imaging Date: Monday, 9 Feb 1998 09:11:16 EST From: MarkCase@aol.com To: rocks-and-fossils@world.std.com Subject: Re: Digital Cameras Sender: rocks-and-fossils-approval@world.std.com Reply-To: rocks-and-fossils@world.std.com Hi Chris and all, I use a Casio QV-30 and love it. It had a Color LCD screen and weighs 9 ounces without the batteries. I use rechargeable batteries and they work great. The only draw back on this camera is that it is a battery hog! That is why I use rechargeables. You can see some of the pictures on my web page: http://members.aol.com/markcase/garnets.htm The price: I bought mine for $299 at office depot. I don't know the retail on it. Mark Case Randleman, NC In a message dated 98-02-09 08:09:09 EST, you write: Stretching the relativity a little, but since there seems to be a proliferation of mineral/fossil websites with varying image qualities, I am interested in getting as much experienced based feedback as possible about digital cameras. If you want to respond directly that's fine or send it to the discussion group. I am interested in performance, brands and $$$$. Thanks, Chris Johnston Subject: How Do You Take Those Pictures Date: Tuesday, 17 Feb 1998 12:31:27 -0600 From: Kevin Ward <themineralgallery@zebra.net> Hi Gary, Sorry it took so long for me to answer your question but you wouldn't believe how swamped I've been with work and filling orders since arriving home. When I take my photos I use a simple love of minerals and my expertise in photography to bring out the best image I can. I use a 35mm manual camera with macro and super macro and natural light. I use 200 speed Kodak film that seems to give the most accurate portrayal of colors and scan the prints into my computer with a UMAX graphics scanner. I then use PhotoShop, PSP, Image Composer, etc., to crop and sharper the image and of course, to compress the memory size. I compare the final image to the mineral and if I'm not happy with the accuracy I redo the scan. Everything you see on the site is 98% accurate to real life and you should be happy with each mineral you purchase from the mineral rooms. I keep getting compliments on my photography so the process seems to be working. Have a good one! Kevin At 03:21 AM 2/15/98 -0500, you wrote: Hi Kevin: I am curious, you have a very well done web page with a great deal of detail in your images of specimens I could expect to quite larger. How do you take the wonderfully detailed and seemingly color-correct photos of the minerals for sale in the 9+ rooms in the Mineral Gallery? What camera are you using? Since it can not be practical to carry a scanner around with you and you can not be at the mercy of the photo processors, can I assume that you are using a digital camera and out putting JPEG files? Next, what is your light source? And just how close can you get to the specimen with your camera? Also, is it safe to assume that you are doing all of your image cropping and web page setups from laptop? What software do you use? Please let me know some more about your images and how you take them, because I am making some big decisions on your material based on what appears to be some very good photography. Thanks, Gary Subject: Digital Imaging Date: Monday, 9 Feb 1998 09:11:16 EST From: D E Russell <russel@spec.net> There's some more info on this at the Digital Camera Resource Page: http://www.dcresource.com Look under the headings for March 4. Good News! A very smart company in California has come up with an ingenious device that is the size of a 35mm film canister and fits in ordinary 35mm cameras. It has a 1.3 million pixel ccd and records up to 30 images to be transferred to your computer. Brilliant! Sounds enticing! Last year a company here in NY announced a similar device for medium format cameras (they were way too pricey for my budget!). It would be great to finally have a digital imaging device with all the features that we've come to love on our 35mm cameras... even if it means using a retrofitted 35mm. Subject: 35mm Camera Digital Conversions Date: Saturday, 28 Mar 1998 09:30:22 -0500 From: D E Russell <russel@spec.net> Gary: I have been told that the new film back insert for 35mm cameras "will sell for under $1,000" Since whenever anyone says that it *never* means a great deal less than $1,000, I presume we mean in the $900 range... possibly with a lower street price. Subject: 35mm Camera Digital Conversions Date: Sunday, 14 June 1998 From: http://www.imagek.com/ IMAGEK web page "Going Digital is a Snap" If you've ever thought of owning a cutting-edge digital camera, IMAGEK has news for you, ---You already own one!--- Fit the IMAGEK EFS-1 electronic film cartridge into the film cavity of your standard 35mm point and shoot or SLR camera and turn it into a digital camera instantly! * 1.3 mega pixel resolution * Doubling the quality of an average digital camera! The system shoots and stores 30 pictures at a time and is reusable up to 100,000 times. Connects to your PC for instant viewing, electronic storage, immediate e-mail transmission and artistic manipulation. Enables custom and standard photos with your printer. One EFS-1 Electronic Film system saves you the expenses of 100,000 rolls of film and processing. Compatible with all standard digital printing methods. Provides creative freedom with your existing lenses and attachments. Allows flexibility to choose between standard 35mm film or EFS format at will. I have not received any more information, price, or first trials of this product. I am interested in reading of if any of you have used this product. Gary ------------------------------------------------------------------------ Another Approach to Digital Close-up Images I have also investigated using Camcorders, VHS or 8mm, to shoot minerals with success. The cameras provide through the lens viewing, zoom magnification to 32x, and can work in low light. I have found that the Raynox Close-up Lens kit woks well on most Camcorders that will accept lens filters. The other benefit to using a Camcorder is the high resolution that each image stream achieves. Of course the draw-back is that the product of a Camcorder is streaming video or a movie. To turn the streaming video or movie into stills on the computer requires another piece of hardware. One can buy a "Snappy" digital video feed hardware editing solution for $199.00, or the Matrox Marvel G200 TV card for $329.00, that connects the computer to the Camcorder for play-back into the computer. I have not tried the "Video Sphinx" but the data sheets provided by the manufacturer states that brilliant snap shots can be captured in high resolution (1600x1200 pixels) from any video source, which is very good. In all cases the ability of the amateur photographer to use household or family video equipment to achieve close-up digital still images that are computer captured is readily achievable and farther advanced than the digital cameras. Certainly, the close-up capacity and magnification factors are farther advanced with video than with digital cameras that I have found. Is this your experience as well? Please share your techniques and observations. Visit http://www.osomin.com/microsco.htm for a complete video technique presentation using a microscope and a $200.00 video conferencing camera in "Video Micro Photography of Minerals On A Budget". Also visit http://www.osomin.com/speciesi.htm for a collection of images using this technique. ------------------------------------------------------------------------ What to Do With Your Slides, Negatives, Prints and Maps Another resource for the photographer with 35mm equipment is the printed photos and slides already shot and processed. To make use of these images and convert them into digital formats that can be read into a computer requires the use of one of two techniques and additional equipment. Minolta, Nikon and other manufacturers make a negative and slide scanner. The Minolta Dimage costs about $600 and scans both slides and strip negatives at 1280x1024 pixels. The Polaroid SprintScan 35 Plus scans positives & negatives, mounted and unmounted chromes at a 2700 dpi resolution, but is expensive at $1,549. While I favor this technique of capturing libraried slides and negatives, I have not yet tried to scan and capture images from my stock shots. The second technique for capturing photos, slides, and maps involves using a VHS or 8 mm camcorder. By placing a camcorder on a tripod or mounted in a copy stand and then arranging peripheral light sources to eliminate glare you are ready to use the close-up capabilities to capture any positive images on video tape. You can do the same thing with slides that are placed on a light box. Once the images are captured on videotape, you have the opportunity to transfer them into your computer via any number of video capture hardware and software components, such as the Snappy, Python, or Sphinx pro. Using the Snappy or similar component will allow you to select one image at a time or to stream them with special effects into your computer. Of course, conventional scanners have been around for many years and color scanners have improved considerably over the past four years. We can now scan almost anything an a flat-bed scanner in 16 million colors with nothing less than exciting detail. For instance the HP 4c scanner cost $1000 two and half years ago and now can be purchased for $485. Like most scanners, it comes with OCR and image software to allow you to scan positive images and text. All of the photos that I have scanned using this method have been superior in detail retention to shooting with a 640x480 pixel digital camera. The drawbacks include the speed of the scanner, setting up for each image scan, and subsequent software handling, but the method works. The convergence of digital and conventional photographic techniques is occurring as I write. Professional photographers have had the ability to shoot conventional film and process the film directly to digital images. The Olympus Digital Photo Studio is an excellent example of this approach and is available for the "casual photographer. If anyone is using a technique like I have described please share some of the particulars, like price, setup, how to use, and what the results look like. ------------------------------------------------------------------------ FRANKLIN & STERLING HILL MINERAL LIST The mineral list has changed significantly over the past four years since the publication of Pete Dunn's five-volume monograph. Some species have been added and others have disappeared from the list without comment. How many changes have you noticed. For instance Basnaesite-group mineral is off the list and Cummingtonite is on; Horneblende is on and Melanterite is off; and there are others. Have you noticed changes in the list? One of the interesting twists of the list is the discussion and verification process of new species to the deposit that is eventually added to the list. It seems that species that we have known for years to be "on the list", verified by reputable sources, discussed at Franklin and often confirmed by the Franklin Mineral Museum may not appear on the list. Such species as Povondraite found at Sterling Hill by Dr. Jenkins, Pyromorphite found at Sterling Hill by Dr. Jenkins, Smythite found at Sterling Hill by Dr. Medreski, and Szaibelyite found at Sterling Hill by Dr. Jenkins are not on the list. Aside from the list published by Dr. Dunn the only other published list is printed in the FOMS Annual Show program. The last list was published in September of 1997 and contained 338 species. I thought there would be more until I noticed some species have been removed. I suppose the removals were made under Dr. Dunn's watchful eye. It is also likely that if you have material in your collection originally purchased or collected under the removed name, you should hold onto the material, since the species may have been moved to the "under study" or "unknown # ?" category such as Hematolite-Like Mineral. Does anybody know for sure? ------------------------------------------------------------------------ Subject: Mineral Changes in the Amphibole Group Date: June 25, 1998 From: The Mineralogical Record, volume 29, May-June 1998 In the article is entitled The Second List of Additions ad Corrections to the Glossary of Mineral Species (1995) by Joseph A. Mandarino the work on and changes in the amphibole group of minerals was discussed. One of the changes of significance to the Franklin and Sterling Hill mineral collector was the mention that Tirodite (p. 170) was no longer a valid species name the manganese magnesium silicate hydroxide. Instead the replacement name is Manganocummingtonite. This article is a fine summarization of the more complex and detailed work presented in the American Mineralogist and other publications. If in your reviews of these published amphibole changes you notice more nomenclature changes relevant to species on the Franklin and Sterling Hill list please bring them to our attention. ------------------------------------------------------------------------ Subject: Call for Papers -- New York Mineralogical Club Date: Wednesday, 3 Jun 1998 16:33:17 -0700 From: minlist@flash.net 1998 George F. Kunz Competition sponsored by the New York Mineralogical Club is open to all authors. Articles about places, people and events within 350 miles of New York City (this includes Virginia to central Maine, all of Pennsylvania, etc.) are eligible for the $500 first prize. For details visit: http://members.aol.com/Jhbnyc/kunz.htm ------------------------------------------------------------------------ Links to other mineral related sites: Mont St. Hilaire http://www.ssc.on.ca/mandm/mshhome.html Mineralogy Club of Antwerp http://www.xs4all.nl/~mineral/index.html Franklin Mineral Museum http://www.geocities.com/CapeCanaveral/Lab/6347/ Herbe Yeates http://super.win.or.jp/~yeates/ Graves Lapidary http://www.rockhounds.com/graves/ Crystallite http://www.crystalite.com/ Bob's Rock Shop http://www.rockhounds.com/rockshop/table.html#maillist Franklin Historical Society http://www.serve.com/FranklinNJ/ Mineralist http://www.serve.com/FranklinNJ/fbnj1.htm Mineral Journals http://www.iem.ac.ru/~dima/geosc/journals/am-min/review/rim_index.html USGS http://minerals.er.usgs.gov/minerals/pubs/product.html Mineralogical Record http://www.minresco.com/minrec/minrec.htm Seamans Museum http://www.phy.mtu.edu/faculty/info/jaszczak/Jaszczak_min.html http://www.geo.mtu.edu/museum/ Bad Boys http://www.paleoart.com/badboys/badboys.htm Kristalle http://www.kristalle.com/index.html Excalibur http://www.bestweb.net/~excalmin/ Parsons http://www.paleoart.com/parsons/parsons.htm UC Minerals http://www.polaris.net/~ucmin/frames.htm OSO Soft Minerals http://www.osomin.com/ The Mineral Gallery http://www.themineralgallery.com/ John Betts Fine Minerals http://members.aol.com/Jhbnyc/home.htm Red Cloud http://www.minrec.org/redcloud.html ------------------------------------------------------------------------ 'Bye for now! --Gary