Introduction
Geodes are nodules (i.e., mineral aggregates having a composition that contrasts strongly with that of the surrounding rock) containing an interior cavity lined with macroscopic crystals (i.e., crystals sufficiently large to be distinguishable without magnification). Geodes occur primarily within limestones, dolomites, and mudrocks, but some are found in volcanic rocks. The term geode is largely synonymous with “vug” (a crystal-lined cavity), but has the additional connotation that the object has, or could, weather free by virtue of its compositional and textural distinctiveness from the host rock. The sizes and shapes of geodes vary widely, but most are in the range of 5 to 10 cm across and roughly spherical or oblate. Geodes are recognized as a group partly on the basis of their appearance and distinctiveness, in particular their attractiveness to mineral collectors. (Figure G2).
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Bibliography
Bassler, R.S., 1908. The formation of geodes, with remarks on the silicification of fossils. Proceedings of the United States National Museum, 133–154.
Boutakoff, N., and Whitehead, S. 1952. Enhydros or water-stones. Mining and Geological Journal, 4(5): 14–18.
Chowns, T.M., and Elkins, J.E. 1974. The origin of quartz geodes and cauliflower cherts through the silicification of anhydrite nodules. Journal of Sedimentary Petrology, 44: 885–903.
Cross, B.L., 1996. The Agates of Northern Mexico. Edina, Minnesota, Burgess International Publishing Group.
Dana, J.D., and Shepard, C.U., 1845. Origin of the constituent and adventitious minerals of trap and allied rocks. American Journal of Science, 49: 49–64.
Elorza, J.J., and Rodriguez-Lazaro, J., 1984. Late Cretaceous quartz geodes after anhydrite from Burgos, Spain. Geological Magazine, 121: 107–113.
Ernst, W.G., and Hall, C.A. Jr., 1975. Feldspathic geodes near Black Mountain, western San Luis Obispo County, California. American Mineralogist, 60: 1105–1112.
Finkleman, R., 1974. A guide to the identification of minerals in geodes from Chihuahua, Mexico. Lapidary Journal, 27: 1742–1744.
Fisher, I.S., 1977. Distribution of Mississippian geodes and geodal minerals in Kentucky. Economic Geology, 72: 864–869.
Foerster, R., 1991. Fossil geodes. Lapidary Journal, 45(3): 102–105.
Goldstein, A., and McKenzie, B. 1997. Halls Gap, Lincoln County, Kentucky. The Mineralogical Record, 28: 369–384.
Hayes, J.B., 1964. Geodes and concretions from the Mississippian Warsaw Formation, Keokuk region, Iowa, Illinois, Missouri. Journal of Sedimentary Petrology, 34: 123–133.
Keller, P.C., 1979. Quartz geodes from near the Sierra Gallego area, Chihuahua, Mexico. The Mineralogical Record, 10(4): 207–214.
Maliva, R.G., 1987. Quartz geodes: early diagenetic silicified anhydrite nodules related to dolomitization. Journal of Sedimentary Petrology, 57: 1054–1059.
Matzko, J.J., and Naqvi, J.M. 1983. Geodes from Saudi Arabia. Lapidary Journal, 37(8): 1140–1156.
Milliken, K.L., 1979. The silicified evaporite syndrome: two aspects of silicification history of former evaporite nodules from southern Kentucky and northern Tennessee. Journal of Sedimentary Petrology, 49: 245–256.
Prashnowsky, A.A., 1990. Biogeochemical study of enhydros (Brazil). Mitteilungen aus dem Geologisch-Palaeontologischen Institut der Universitaet Hamburg, 69: 35–43.
Radke, B., and Nicoll, R.S. 1981. Evidence for former evaporites in the Carboniferous Moogooree Limestone, Carnarvon Basin, Western Australia. BMR Journal of Australian Geology and Geophysics, 6(1): 106–108.
Robertson, P., 1942. Bituminous matter in Warsaw geodes [Illinois]. Transactions of the Illinois State Academy of Science, 35: 138–140.
Roedder, E., 1979. Fluid inclusion evidence on the environments of sedimentary diagenesis, a review. In Scholle, P.A. and Schluger, P.R. (eds.), Aspects of Diagenesis. Tulsa, Oklahoma, SEPM, 26: pp. 89–107.
Shaler, N.S., 1899. Formation of dikes and veins. Geological Society of America Bulletin, 10: 253–262.
Siedlecka, A., 1976. Silicified Precambrian evaporite nodules from northern Norway; a preliminary report. Sedimentary Geology, 16: 161–175.
Sinotte, S.R., 1969. The Fabulous Keokuk Geodes-M Volume 1. their origin, formation, and development in the Mississippian lower Warsaw beds of southeast Iowa and adjacent states. Des Moines, Iowa, Wallace-Homestead Co.
Spitznas, R.L., 1949. Petroliferous geodes, their occurrence and origin [Tyson Creek area, Illinois]. Earth Science Digest, 3(11): 15–18.
Ulmer-Scholle, D.S., Scholle, P.A. et al., 1993. Silicification of evaporites in Permian (Guadalupian) back-reef carbonates of the Delaware Basin, West Texas and New Mexico. Journal of Sedimentary Petrology, 63: 955–965.
Van Tuyl, F.M., 1916. The geodes of the Keokuk beds. American Journal of Science, 42(192): 34–42.
Cross-references
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1978 Dowden, Hutchinson & Ross, Inc.
About this entry
Cite this entry
Milliken, K.L. (1978). Geodes. In: Middleton, G.V., Church, M.J., Coniglio, M., Hardie, L.A., Longstaffe, F.J. (eds) Encyclopedia of Sediments and Sedimentary Rocks. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3609-5_96
Download citation
DOI: https://doi.org/10.1007/978-1-4020-3609-5_96
Published:
Publisher Name: Springer, Dordrecht
Print ISBN: 978-1-4020-0872-6
Online ISBN: 978-1-4020-3609-5
eBook Packages: Springer Book Archive