[CZ]
Souradnice vas privedou na misto, kde na povrch usti (vyvera)
podzemni vodni tok. Takovemu mistu se rika vyver nebo tez
vyveracka. Opakem vyveru je ponor, coz je misto, kde
se povrchovy tok zanoruje do podzemi. Ponorum se venuje napr.
earthcache
Ponory Ricky (GC1HNPR).
Vyvery i ponory se obvykle nachazeji v krasovych oblastech.
Jednim z mist Moravskeho krasu, kde lze vyvery pozorovat, je
Josefovske udoli. Zde si predstavime pet
nejvyznamnejsich.
Vyvery Jedovnickych vod
(1)
Jedna se o system tri vyveru, kterymi se (po 5km podzemniho toku od
Rudickeho propadani) dostava Jedovnicky potok opet do
povrchoveho koryta. Tyto vyveracky se nachazeji 200m zapadne od
Byci skaly. Puvodne zde byl aktivni pouze jeden vyver, zbyle
dva byly otevreny nahodou v lomu, ktery s vyverackou bezprostredne
souvisi. Tyto vyvery behem posledniho stoleti vyznamne zmenili
svoji podobu, nebot jsou znacne poznamenany tezbou kamene.
Olomucansky vyver (2)
Silny pramen z neznamych jeskynnich prostor je od vyveru
Jedovnickeho potoka vzdalen 300m zapadne. V roce 1928-1929
byl vyver upraven jako zdrojnice pitne vody pro Adamov.
Vyver naproti Jachymce
(3)
Nachazi se pod vapencovou skalou nedaleko jeskyne Jachymka a
castecne zasahuje do silnice. Nachazi se asi 400m zapadne od
Josefova. Potucek vyvera pod silnici, v lete je mozne misto
poznat podle bujnejsi vegetace.
Vyvery u Svycarny (4)
Dalsi z vyveru v Josefovskem udoli se nachazi naproti
Stare huti, nedaleko od Svycarny. Vyvera z vapencove
strane, ktera je od zbytku vapencoveho Josefovskeho udoli
jiz oddelena brnenskou vyvrelinou. Puvodne potok vyveral z male
jeskyne, kterou dal majitel majitel blizkeho domku upravit na
sklep, v soucasne dobe voda usti na povrch zeleznou trubkou a
pramen je upraven na studanku.
Vyvery Krtinskeho potoka
(5)
Jedna se o system ctyr vyveru. Prvni je povodnovy vyver, ktery
tvori slepe rameno vetsinou vyschleho potoka. Druhym je spojeny
vyver a propadani zvany Otevrena skala, kde potok vyvera a
zase se straci. To vzniklo utrzenim skalniho bloku pri stavbe
silnice. Dalsi z vyveru byl stavbou silnice obnazen, nasledne zase
zasypan a v soucasne dobe je vytok spatne patrny, zakryty mostem.
Posledni vyver se nachazi pod jeskyni Kostelik.
Ukoly nutne pro
zalogovani:
1. K logu prilozte svoje foto s GPS
(samostatnym lovcum staci foto jejich GPS) u vyveracky na
startovacich souradnicich.
2. Na muj email odeslete odpovedi na nasledujici otazky:
a) Jaka je nadmorska vyska kamenu u
vyveracky (viz. obrazek)?
b) Kam se vleva Jedovnicky potok?
c) Jakou byla barva vyverajici vody v dobe
vasi navstevy?
Necekejte na potvrzeni a rovnou se zalogujte. Ozvu se pouze v
pripade chybne odpovedi.
Zdroje informaci: Informacni materialy Spravy CHKO Moravsky
kras
[EN]
The coordinates will lead you to the place where underground water
stream stems rises to the surface. Such a place is called karst
spring. The opposite of karst spring is ponor, which is
the place where the water stream flows to the underground. E.g. the
Ponory Ricky / Ponors of the Ricka river(GC1HNPR)engages
in ponors.
Karst springs and ponors can usually be found in karst areas.
One of the places in the Moravian Karst where karst springs can be
observed is Josefov valley. We will present five most
important carst springs.
Karst springs of Jedovnice
waters (1)
This is a system of three karst springs through which (after 5km of
underground water from Rudice pit) the Jedovnice
creek comes to the surface riverbed again. These karst springs
can be found 200m to the west of Byci skala. There used to
be only one active karst spring, the other two happen to be open in
the quarry that is directly connected with the karst spring. These
karst springs changed significantly during the last century due to
the stone mining.
Karst spring of Olomucany
(2)
A strong stream from unknown cave space can be found 300m to the
west from the karst spring of Jedovnicky creek. In 1928-1929
the karst spring was adjusted as a source of water for
Adamov.
Karst spring across from
Jachymka (3)
It can be found under a limestone rock near the Jachymka
cave and stretches partly into the road. It is located about
400m to the west of Josefov. The creek rises under the road,
in summer you can discover the place according to a more luxuriant
vegetation.
Karst springs near Svycarna
(4)
Another of the karst springs in Josefov valley is located
across from the Stara hut (Old ironworks), near
Svycarna. It rises from a limestone hillside which has been
separated from the rest of the limestone Josefov valley by
Brno volcanic rock. The creek used to rise from a small cave, which
the owner of a near house had adjusted as a cellar, now water flows
to the surface through an iron pipe and the spring has been
adjusted as a well.
Karst springs of Krtinsky
creek (5)
This is a system of four karst springs. The first one is a flood
karst spring which creates a blind branch of a creek that mostly
runs dry. The second karst spring connected with pit is called
Otevrena skala (Open rock) where the creek rises and
disappears again. This was created due to a rock block that broke
off during the road construction. Another of the karst spring was
uncovered during the road construction, later covered on again and
now the karst spring is hardly visible, covered with a bridge. The
last karst spring is located under the Kostelik cave.
The necessary tasks for
logging:
1. Add your photo with a GPS made near the
karst spring at the start coordinates (for alone cachers a photo of
their GPS will do).
2. Send answers to the folowing questions to my e-mail:
a) What is the altitude of the stones at
the karst spring (see the picture)?
b) Where does the Jedovnicky creek flow
into?
c) What colour was the water during your
visit?
Source of information: Information materials of
Administration of the Moravian Karst Protected Landscape
Area.