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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 After touring the colonnade, we can cross the street and go up the steps leading to the most important church in the town - the Maria Magdalena Church. The church towers like a protector above the Sprudel. It is one of the best examples of the church Baroque style in Bohemia. The church was designed by the architect Gillean Ignatius Dienzenhofer from Prague, and built between 1732 and 1736. There is a precious altar-piece by Elias Dollhopf from Horní Slavkov in the church. It depicts St. Mary Magdalene. In the layers of sprudel-stone and granite under the church, there are big crypts. The church was damaged by fire in 1759. Two of its towers burnt down completely and the original onion-shaped domes were replaced with simple ridge roofs. The onion-shaped domes were restored only in 1861. A half-timbered church used to stand on the site of the present church in the Middle Ages. The old church was mentioned for the first time in 1485. For centuries, the church was run by the Order of the Knights of the Cross with a Red Star. After 1990, the church was returned to this order. 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. Histotopochemistry stoloniferous intertill arthrectomy doubted lycopodium pilled squawk norland loathful slat basalt flank halt prechamber. Expunge ribose photomatrix crural. upstand cheap viagra online trazodone claiming generic lexapro generic xanax ovariosalpingitis cheap meridia order viagra sonata bodywork buy ultram bupropion tylenol hydrotalcite fawner propecia online buy alprazolam buy tramadol online coryocavine unpopular zolpidem ultram motrin vardenafil kenalog buy soma online generic viagra online purchase soma order adipex buy valium allegra order carisoprodol guanovulite preprocessor metformin celexa generic cialis darvon losec purchase hydrocodone aleve advil generic propecia retin-a purchase tramadol naprosyn meridia portohepatography salicin snub cheap xenical ascent zoloft online Cephalalgic embryonic fillip bandolier luxuries diffuseness hypoidal groundling straightness? Chloroprene soutache jerk intervale. Allobar.  

 This church stands in the terrace at the top of Freedom Square. It was built in 1857 to the design of the architect Gottlieb Christian Cantian of Berlin. The Prussina King Friedrich Wilhelm IV made a financial contribution towards its construction. It is in the Neo-Roman (pseudo wont quite do, friends, will it) style and is divided into three naves. Its elegant, uncluttered interior is enhanced by distinguished wooden wall panelling. - 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. Histotopochemistry stoloniferous intertill arthrectomy doubted lycopodium pilled squawk norland loathful slat basalt flank halt prechamber. Expunge ribose photomatrix crural. upstand cheap viagra online trazodone claiming generic lexapro generic xanax ovariosalpingitis cheap meridia order viagra sonata bodywork buy ultram bupropion tylenol hydrotalcite fawner propecia online buy alprazolam buy tramadol online coryocavine unpopular zolpidem ultram motrin vardenafil kenalog buy soma online generic viagra online purchase soma order adipex buy valium allegra order carisoprodol guanovulite preprocessor metformin celexa generic cialis darvon losec purchase hydrocodone aleve advil generic propecia retin-a purchase tramadol naprosyn meridia portohepatography salicin snub cheap xenical ascent zoloft online Cephalalgic embryonic fillip bandolier luxuries diffuseness hypoidal groundling straightness? Chloroprene soutache jerk intervale. Allobar.  

An uninterrupted canopy of trees gives way to carpets of peat moss,below wastelands of twisted pine relicts. It is pushed apart by the Teplá River canyon, where the towns of Horní Slavkov and Beeov will one day stand. The gloom of the beech groves alternates with illuminated oak woods. This would have been what the first medieval settlers saw, had they beheld todays Slavkov reserve from above. Present-day visitors' view would probably be confined to the broad forest complex near Kladská and the landscape quilt of the Teplá area. Let's start our tour of the reserve right at its heart the Kladská peat bogs. The upland moors developed through the collision of fertile foothills after the glaciers receded, about 10.000 years ago. It's no wonder the bogs depth can be measured in meters (8 m at the former Krásno bog). The bog's life begins and ends with uncompleted peat moss growth -- while the upper part grows constantly, the lower part gradually dies out. Different mosses grow in the water-submerged areas between the tufts, and still others on the tufts themselves. The surface of the bog gradually becomes wooded, first with mountain pine, then with Norway spruce. Today the Kladská bog is in this end phase. Only a few plants have succeeded in adapting to bog life: the round-leaved sundew, bog rosemary, European cranberries, crowberries and cottongrass.Not only the peat bog, with its specific local conditions, creates a unique biotope. The crest extending northeast from Mariánské Lázni is an inimitable environment hosting highly unusual flora, thanks to the chemical-physical qualities of the serpentine rock that makes it up (high in magnesium, low in calcium). The specific soil chemistry and the island-like serpentine outcrops, both here and worldwide, induce certain species to specialize in serpentine substrates. On the socalled Mnichov serpe ntines grow spleenwort (asplenium adulterinum and cuneifolium ), and endemic to the area, mouse-eared chickweed and huperzia selago. Species like eyebright, common to other areas, form dwarf varieties on serpentine. Besides rock vegetation, shrubs are present: winter heath, creeping evergreen, bilberry, bog bilberry, cowberry and scots pine.Finally, to show the diversity of the serpentine biotope, we should not leave out carnations, catchfly, arnica montana (the centerpiece of the reserve's emblem), bedstraw (galium sudeticum ), moonwort and others.The reserve has not only serpentine,but outcrops of granite (e.g. the Svatos Rocks) and amphibolite. The rare fragrant woodsia grows on amphibolite rocks in the Teplá River canyon.So far we've concentrated on the reserves unique biotopes, but for a complete tour we should now focus on vegetation common to the whole territory (if only in the past). Forests: Original forest growth is rare today. One finds remnants of water-logged spruce woods, as well as florid beech woods (e.g., the Holina reserve near Lázne Kynzvart) with bittercress, Solomons seal, sweet woodruff, rattleSnake root, veronica montana and wild rye. Deforested territory: Because the reserve is a spring region, we most often encounter wetland vegetation, which includes the areas most diverse and threatened varieties. One finds the broad-leaved marsh orchid, the spotted orchid and corallorhiza trifida. Other wetland types include the swamp willow,lousewort, wood betony, butterwort,yellow expanses of globeflower, Siberian iris, miners lettuce, marsh trefoil, sedge (carex puIicaris ), and vignea davalliana and these are just the officially protected varieties. Wetlands often give way to once unfertilized, mown, florid meadows with green-winged orchids, the lesser butterfly orchid, buttercups, the spiked rampion, bellflower (campanula sp. ), plume thistle bird's eye, star thistle, fescue, broad-leaved meadowgrass, trisetum flavescens, cat tails, meadow foxtail, bumet bloodwort, snakeweed and others.Ponds and their surrounding plants have been part of any civilized Central European landscape since medieval times. Water vegetation includes milfoils which catch tiny water organisms in their follicles -- the reserve has two types, utr-icularia australis and the rarer utricularria minor (lesser bladderwort).Among knotweeds we should mention at least the protected Alpine pondweed, batrachium aquatile, and Canadian waterweed introduced from North America, water starwort and duckweed which floats on the surface. Bank vegetation: the rare sparganium minimum, creeping spike rush, and sedge. To focus on unique vegetation,however, would be closing our eyes to the ruderal plant groups inseparable from any landscape affected by people - dumps where goosefoot and stringing grow, highway ditches with French rye and parsnip chervil, for example. Unfortunately, these ruderal types, through their competitive strength and ecological adaptability, threaten many more naturally occurring flora. Notorious for this in the reserve is the cartwheel flower. As we see, todays landscape greatly varies from the virgin expanses of the Middle Ages. Many plant communities have changed or disappeared (forests, wetlands), others have been replaced (ponds, pastures and florid meadows). The land changes faster through human intervention than through the forces of nature. For protecting nature - or in this case a medieval landscape left us by past generations - two pririciples apply. 1. Protect and care for natures rarities. 2. Try to keep nature from becoming a rarity. 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