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Field CollectingOklahoma
26th Feb 2018 18:53 UTCKevin Conroy Manager
26th Feb 2018 19:57 UTCPaul Brandes 🌟 Manager
26th Feb 2018 22:40 UTCKevin Conroy Manager
27th Feb 2018 01:55 UTCVma Buck
27th Feb 2018 18:05 UTCDave Barnard
"Below the plains, ground water travels through the salt-saturated sand and comes to the surface where it evaporates, leaving the crust of salt. The concentrated saline solution combines with gypsum to promote selenite crystal growth in a portion of the salt flats. Selenite is a crystallized form of gypsum. Chemically, it is a hydrous calcium sulfate. Gypsum is a common mineral that takes on a great variety of crystal forms and shapes. On the Salt Plains, the crystals are formed just below the salt encrusted surface. They are seldom found deeper than two feet below the surface. Crystals take on the characteristics of their environment; the finer the soil, the more clear the crystals. Iron oxide in the soil gives the crystals their chocolate brown color."
https://www.fws.gov/refuge/Salt_Plains/about/selenite.html
27th Feb 2018 18:23 UTCBob Harman
No exceptions and nothing permitted other than these dates as the area is otherwise reserved for Whooping Cranes during their spring and fall migrations. CHEERS.....BOB
8th May 2018 16:39 UTCScott DeLano
Trilobites at Black Cat Mountain...but I do not know if they let people in or not. It may be private property.
Tripoli mineral just west of Seneca, MO on the Oklahoma side of the border.
Lots of black shale areas in NE Oklahoma where you can find pyrite / marcasite crystals.
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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 24, 2024 06:20:29