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228541
LocalitiesOld Saybrook, Middlesex County, Connecticut, USA
24th Jan 2012 23:19 UTCHarold Moritz 🌟 Expert
Here is the text from Robinson regarding minerals from Saybrook:
Epidote, crystallized.
Apophyllite; near.
Actynolite.
Anthophyllite. This rare mineral is said to have been found near this town.
Chlorite, in small crystals.
Sillimanite. This mineral, previously called anthophylite, is of a dark grey color, passing into clove brown. It occurs in rhomboidal prisms. It has but one cleavage, which is parallel to the longer diagonal of the prism. The sides and angles of the crystals are frequently rounded. It is harder than quartz,—found in a vein of quartz penetrating gneiss. (Sil. 8.113.) This locality is on the turnpike leading from Saybrook to Middletown, not far from 2 1/2 m. beyond the locality of molybdena, in the parish of Chester, on the left hand of the path, in a flat rock which is chiefly mica slate, a few rods S. of the Post Office, which is kept in a room of Denison's tavern, near a small stream running into the Connecticut—crystallized in veins of quartz. (Sil. 8.195.) The writer is informed that the above mineral was previously named in Europe, and has been since known there by the name of Mc Clellanite.
Sulphuret of Molybdena, a small distance northerly from Pettypaug m. h. in a vein of quartz traversing gneiss, (C.) ½ a m E. of the Middletown turnpike, near the house of the Widow Pratt, on the first road on the right hand, above the turnpike gate. (Sil. 1.242.)
The epidote and chlorite localities are uncertain, as is the actinolite, though they are plausible given the metamorphic terrane here. At best these should be attributed to Middlesex County as they could be from a number of towns. Anthophyllite is erroneous (as reported by Bowen in his 1824 type description, this is what the sillimanite crystals were thought to be previously) and apophyllite is very likely a confusion with anthophyllite as the right rocks for apophyllite do not occur here and it has never been found in the area since.
What is certain is that the sillimanite locality description is the type locality, now in Chester, and the molybdenite locality is now in Essex. Mindat pages for these will be created. I visited the sillimanite type locality today and it is in the very center of town and now completely developed, no outcrops are evident. Even in 1817 when it was found the area would have been developed). However, the person who provided Bowen with the locality information said it was "in a flat rock" that is "mica slate" (schistose gneiss) and there are still abundant loose slabs of gray gneiss of the Tatnic Hill Formation along Pattaconk Brook and in stone walls in the immediate area. I believe the crystals were in a loose slab and not in an outcrop.
25th Jan 2012 00:59 UTCPeter Cristofono
Thanks for doing all of this research and for your field report on the sillimanite type locality!
Best,
Peter
25th Jan 2012 02:29 UTCHarold Moritz 🌟 Expert
25th Jan 2012 02:39 UTCPeter Cristofono
I'll make an inquiry for you.
25th Jan 2012 19:36 UTCHarold Moritz 🌟 Expert
27th Jan 2012 14:58 UTCPeter Cristofono
The Harvard Museum database for this specimen only indicates that it is sillimanite from Chester. Unfortunately, there is no other information. Not sure what the red stuff, is - looks to me like iron oxide. I'd have to take a look again at the specimen (it's down in the basement storage area) to tell you more. Next time I'm there, I'll check it out.
Peter
27th Jan 2012 17:41 UTCHarold Moritz 🌟 Expert
I have never seen any other reference to any other mineral locality in Chester. As the specimen is only labeled "Chester" it must be type material, sure looks like it. Date of acquisition and from whom would help.
Thanks
Fritz
28th Jan 2012 01:35 UTCPeter Cristofono
The 85xxxx specimen number means that it must have been acquired by Harvard in the early 1920s. For example, #86694 (ruby) was acquired in 1925; and #89815 - rhodonite - was field collected in 1927.
Compare this Harvard specimen of "Chlorophyllite" from its type locality, # 85305. It was in the collection of JD Whitney (1819-1896) so it was a nineteenth century specimen, but the 85xxxx indicates that it was acquired around the time of the sillimanite specimen.
Peter
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Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2024, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: April 26, 2024 10:35:08