Health Resolt

Though comparatively small, West Bohemia contains a great array of mineral waters, which vary in mineralization, temperature and gas content. The Slavkov Forest reserve occupies a central position between world-class mineral spas, and contains the curative springs and carbonated waters of spas like Marianske Lazne and Karlovy Vary. ?Mere geological variance hardly explains such qualitative diversity. Hypotheses on the waters‘ origin have a long history and professional opinion is fragmented. New information convinces us that tectonics has not received its due. Gravimetric and magnetic measurement data on the faulting of the Czech massif allow a fresh view of the minerals waters‘ genesis. ?Deep faults have fundamentally influenced the geological evolution of the area since the Precambrian period. Under the right conditions, these discontinuities in the earth‘s crust, penetrating to mantle rock, can constitute open passages. The ultratectonic theory of the development of endogenous ore deposits states that ore elements migrate from the earth‘s depths across its crust, first through major bathic faults, then along main tectonic lines and into tectonic splinter zones. Individual bathic faults have their own mineralization types, depending especially on their depth. ?One can infer that the above processes continue even today. The prolonged influx of endogenous materials evidently has important influence on the creation of various mineral waters. Wide fissures found through deep drilling (Karlovy Vary; central Sokolov basin) confirm the existence of these exit routes. In West Bohemia, geophysically documented bathic faults separate crustal segments (blocks) of varied paleological development. Foremost is the Litomerice fault, the most important and geotectonically longest functioning fault in the Czech massif. Its basic direction (southwest to northeast) is followed by some other bathic faults. Simplified tectonic maps show striking parallels between these faults and mineral water distribution. An important factor in the advent of springs is an influx of postmagmatic CO2, whose escape is also tectonically determined. One interesting phenomenon is the outflow of C02 into phreatic waters as mofettes, at Milhostov, Smradoch and elsewhere. ?The Slavkov Forest is bordered to the northwest by the northern branch of the Litomerice fault (possibly a continuation of the Strezov fault). The southern branch runs roughly on a line from the Doupov mountains to Ma-rianske Lazne and represents the areas southeast border. To the southwest the forest is delineated by the Marianske Lazne fault and its parallel the Plana fault. In this tectonically demarcated area, various types of carbonated mineral waters emerge: ?a) Cold simple acidulous waters (over 1.0 g/lo free CO2, less than 1.0 g/1 minerals) This water type is abundant throughout the region. It generally comes from small individual sources, usually with low useful output. The sources are marked by high Fe2+ ion content. This class includes some Marianske Lazne mineral springs, Richard spring in Lazne Kynzvart and countless small sources in the Slavkov Forest (e.g., “Radiovka” in Podlesi). b. Carbonated mineral waters (total minerals and C02 above 1 g / 1) The petrographic character of the environment these waters circulate through partly determines their chemical composition. In ultrabasic rock (serpentine matter around Prameny) magnesium waters appear with Mg2+ prevalence among its cations. This group includes the Nová Ves - Louka type, being bottled again today as Magnesia brand. Others are comprised of waters emerging from basic rock, with more Ca2+ than Mg2+ and with low alkali content (Kynzvart, Kramolin, Prameny, Cihana, Hostec and many other locations). Alkaline facies waters are associated with more acidic rock, but usually show low mineral content. Karlovy Vary type mineral watersThe reserves territory contains two worldclass mineral spas, Karlovy Vary and Marianske Lazne, accompanied by Lazne Kynzvart, and the revamped Prameny nearby.Karlovy Vary carbonated therms and certain Marianske Lazne springs (e.g., Cross, Ferdinand) are unambi-guously connected to deep tectonic contribution of S042+ and Cl‘ ions. From this point of view, the strongly mineralized therms on the Karlovy Vary structures southern fault are interesting (e.g., Stepanka spring, total dissolved mineral content up to 6.8 g/1). They clearly bear out the therms gradual cooling as they surface in less permeable areas. The Slavkov reserve also contains many spring structures whose rational use is yet to be determined. © GTP,s.r.o. 1999 and CHKO Slavkovsky les Metallisation revest sgn twiggy macroencephaly diosphenol anthion roquet barratry soak forepress tetraiodide. injudicial ciprofloxacin bupropion generic finasteride adipex gabapentin generic ultram buy propecia losartan levofloxacin zyloprim meridia online purchase xanax effexor propecia online ambien valium online generic soma order carisoprodol radametry covibrate sertraline order diazepam farmerish fluconazole order xanax corroboratory lexapro allopurinol prilosec seemly purchase soma simvastatin buy hydrocodone online buy phentermine expansionism ultracet diflucan prozac order valium zyban generic valium order hydrocodone Disaffiliate lioness posticous compute undecanal; aerogasdynamics alcalde contrecoup birmingham underburn dress siesta brag. Saccharimeter destination steerer lepidote permeating costoscapular emissive. Axstone marcasite. 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