Peloid

From Wikipedia, the free encyclopedia
For the geologic term, see peloids.
Family of African Bush Elephants taking a mud bath in Tsavo East National Park, Kenya.

Peloid is mud, or clay used therapeutically, as part of balneotherapy, or therapeutic bathing. Peloids consist of humus and minerals formed over many years by geological and biological, chemical and physical processes.

Numerous peloids are available today, of which the most popular are peat pulps, various medicinal clays, mined in various locations around the world, and a variety of plant substances. Also, health spas often use locally available lake and sea muds and clays. Peloid procedures are also various; the most common of them are peloid wraps, peloid baths, and peloid packs applied locally to the part of the body, which is being treated.

Peloid packs and, specifically, peat, have been used in Europe for medicinal baths and wraps for the past 200 years.

Peloid preparation varies in different spas. Typically, peloids are matured for a period of up to 2 years in special ponds.

"The majority of spas ... use artificial ponds where the natural ("virgin") clay is mixed with mineral, thermo-mineral, or sea water that issues in the vicinity of the spas or inside the spa buildings."[1]

Peloid treatments have been used for rheumatic disorders, osteoarthritis, gynecological disorders, sciatica, skin diseases, trauma and many more various afflictions and ailments.

Peloids are widely used in cosmetology. They are applied as face masks. Applying peloid masks once a week helps to revitalize the skin, tighten it and bind fluids in the skin layers. Regular use of peloids cause wrinkles to disappear and prevents new wrinkles from appearing.

See also

Notes

  1. ↑ Carretaro MI, Gomes CSF, Tateo F. "Clays and human health." In: Bergaya F, Theng BKG, Lagaly G, editors. Handbook of Clay Science, Developments in Clay Science. Vol. 1. Elsevier Ltd; Amsterdam: 2006. pp. 717–741. ISBN 0-08-044183-1, ISBN 978-0-08-044183-2 p. 724

References

This article is issued from Wikipedia. The text is available under the Creative Commons Attribution/Share Alike; additional terms may apply for the media files.