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        <div id="content-top1">Page 8 - LZ April 2017</div>
        <div id="content-top2">P. 8</div>
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    <pre style="white-space:pre-line"><code>Butkov - prÃ­loha

Butkov                                                                             Foto: Lom Butkov v roku 1935
a KaliÅ¡te
pamÃ¤tajÃº
more

Butkov â€“ ÄastÃ¡ tÃ©ma pre vedcov, technikov, mÃ­nerov, strojnÃ­kov, laborantov, robotnÃ­kov. LadÄiansky lom â€“ zdroj kvalitnÃ©ho
vÃ¡penca na kvalitnÃ½ portlandskÃ½ cement sa neustÃ¡le menil. Za relatÃ­vne krÃ¡tky Äas jeden a Å¡tvrÅ¥ storoÄia i v relÃ¡ciÃ¡ch de-
siatok miliÃ³nov rokov. ZaÅ¾il Äas diluviÃ¡lneho mora, Äasy dobÃ½vania obyÄajnÃ½mi nÃ¡strojmi i modernÃ½mi mechanizmami,
Å¾elezniÄku Å¥ahanÃº konÃ­kmi aj modernÃ½ dopravnÃ­k.
Butkov zamestnÃ¡val a Å¾ivil mnohÃ© generÃ¡cie a Å¾iaÄ¾, aj vyhasil Å¾ivot dvadsiatky robotnÃ­kov.
Pre Butkov, jeho modernizÃ¡ciu, zvyÅ¡ovanie vÃ½konov Å¡edivelo mnoho zodpovednÃ½ch pracovnÃ­kov. Proces zlepÅ¡ovania a
zefektÃ­vÅˆovania je tu aj teraz a zrejme nikdy neskonÄÃ­.
OdhalenÃ½ Butkov je dominantou Ladiec a urÄite zostane Åˆou dovtedy, kÃ½m sa bude vyrÃ¡baÅ¥ cement.
V ostatnÃ½ch rokoch dostal Butkov i duchovnÃ½ rozmer â€“ vstÃºpil do vedomia veriacich a v poslednom Äase aj turistov a
Å¡portovcov.

Vizitka                                 zmene podmorskej erÃ³zie a vytvÃ¡-
                                        rali sa masy brekciÃ­ (pevnÃ¡ usadeni-
Vrch Butkov (765 m n.m.) vÃ½raznÃ¡        na z hornÃ­n, nerastov a skamenelÃ­n).
morfologickÃ¡ lokalita na zÃ¡padnom       Komplex sa rozdelil na Å¡tyri sÃºvrstvia:
okraji StrÃ¡Å¾ovskÃ½ch vrchov. Na seve-    ladÄianske, mrÃ¡znickÃ©, kaliÅ¡tianskÃ© a
ro-zÃ¡padnom svahu je lom otvorenÃ½       lÃºÄkovskÃ©.
v rokoch 1888 â€“ 1889. SystÃ©m dolova-    IlavskÃ¡ kotlina, v ktorej sa nachÃ¡dza
nia je etÃ¡Å¾ovÃ½ a mÃ¡ vÃ½Å¡ku 330 metrov    naÅ¡a obec, vznikla v obdobÃ­ neogÃ©-
(od 350 m n.m. do 680 m n.m.).          nu (pred 13 miliÃ³nmi rokov). Jej dÄºÅ¾-
Butkov susedÃ­ s vrchom KaliÅ¡te          ka je 30 km, Å¡Ã­rka 2 â€“ 5 km. Rozloha
(675 m n.m.), na ktorÃ©ho Äasti StrednÃ¡  je pribliÅ¾ne 150 km2. CelÃ¡ oblasÅ¥ mÃ¡
hora je vÃ¡pencovÃ½ lom.                  erÃ³zno-tektonickÃ½ pÃ´vod, najmÃ¤ Äin-
                                        nosÅ¥ou rieky VÃ¡h.
Vedci o Butkove a KaliÅ¡ti
                                        Butkov a KaliÅ¡te
SlovenskÃ¡ akadÃ©mia vied vydala v        pamÃ¤tajÃº more                              je z TuneÅ¾Ã­c. VÃ½znamnÃ½mi obyvateÄ¾mi
roku 2013 v sponzorstve PovaÅ¾skej                                                  druhohornÃ©ho mora boli amonity â€“
cementÃ¡rne, a.s. vedeckÃº publikÃ¡ciu     Autori spomÃ­nanej publikÃ¡cie o Butko-      hlavonoÅ¾ce pohybujÃºce sa reaktÃ­vnym
â€žVrch Butkov, kamennÃ½ archÃ­v histÃ³rie   ve opisujÃº jednobunkovÃ© organizmy a        spÃ´sobom. NaÅ¡li sa na svahoch Hradis-
slovenskÃ½ch vrchov a druhohornÃ©ho       Å¾ivoÄÃ­chy â€“ obyvateÄ¾ov druhohornÃ©ho        ka, Strednej hory, KaliÅ¡Å¥a i Butkova. Na
morskÃ©ho Å¾ivotaâ€œ (autori Jozef Micha-   mora, z ktorÃ½ch niektorÃ© nÃ¡jdeme aj        Butkove predstavujÃº najbohatÅ¡iu loka-
lÃ­k a ZdenÄ›k VaÅ¡Ã­Äek).                  v dneÅ¡nÃ½ch oceÃ¡noch. VÃ¤ÄÅ¡ina z nich        litu v ZÃ¡padnÃ½ch Karpatoch.
V knihe sa okrem histÃ³rie cementÃ¡r-     mÃ¡ mikroskopickÃ© rozmery, ale niek-        V druhohornÃ½ch moriach Å¾ili aj ryby a
ne zaoberajÃº najviac geolÃ³giou vzni-    torÃ© sÃº aj niekoÄ¾ko centimetrov veÄ¾kÃ©.     Å¾raloky. PoÄas 300 miliÃ³nov rokov sa
ku sÃºstavy, v ktorej sa nachÃ¡dza vrch   Sem patrÃ­ nanoplanktÃ³n, skupina jed-       vÃ½voj Å¾raloka vÃ½raznejÅ¡ie nezmenil.
Butkov.                                 nobunkovÃ½ch organizmov s vÃ¡penco-          ZvyÅ¡ky skamenelÃ­n sÃº pomerne zried-
VeÄ¾a miesta venujÃº svedkom dÃ¡vnej       vou schrÃ¡nkou. BiÄÃ­kovce â€“ jednobun-       kavÃ©. Z lokality Butkov boli k dispozÃ­cii
minulosti, organizmom a Å¾ivoÄÃ­chom,     kovÃ© Å¾ivoÄÃ­chy spÃ¡jajÃºce vlastnosti        tri neÃºplnÃ© zuby.
ktorÃ© Å¾ili v druhohornom mori a ich     rastlÃ­n a Å¾ivoÄÃ­chov. Dierkavce â€“ sÃº tieÅ¾  PodÄ¾a pracovnÃ­kov Slovenskej akadÃ©-
skamenelinÃ¡m, ktorÃ© sa nachÃ¡dzajÃº       jednobunkovÃ© Å¾ivoÄÃ­chy (prvoky), kto-      mie vied patria Butkov a KaliÅ¡te medzi
na Butkove a KaliÅ¡ti.                   rÃ© majÃº veÄ¾kÃ½ horninotvornÃ½ vÃ½znam         najvÃ½znamnejÅ¡ie lokality tohto druhu
                                        â€“ masovÃ© nazhromaÅ¾denie ich schrÃ¡-         pre bÃ¡danie vedcov.
OdkiaÄ¾ priÅ¡li vrchy                     nok vedie k vzniku vÃ¡pencov. Rovnako       TakÃ½to pohÄ¾ad na neuveriteÄ¾ne dÃ¡vnu
                                        pÃ´sobili aj tintinidy.                     minulosÅ¥ Butkova a KaliÅ¡Å¥a nÃ¡m pred-
Pred 200 miliÃ³nmi rokov uloÅ¾eniny       ÄŽalÅ¡ia skupina Å¾ivoÄÃ­chov, ktorÃ½ch ska-    stavÃ­ vrchy, na ktorÃ© sa denne dÃ­vame
tej doby sa vyskytujÃº v okolÃ­ Tren-     meneliny sa naÅ¡li na Butkove a Stred-      v zloÅ¾itej, miliÃ³ny rokov trvajÃºcej pre-
Äianskych TeplÃ­c, Butkove a ManÃ­ne.     nej hore sÃº hubky a ramenonoÅ¾ce. ÄŽa-       mene.
NajstarÅ¡ie sÃº tuneÅ¾ickÃ© vÃ¡pence vy-     lej sÃº to lastÃºrniky, trieda mÃ¤kkÃ½Å¡ov,
stupujÃºce na najvyÅ¡Å¡ie poloÅ¾enej Äas-   ktorÃ½ch typickÃ½m znakom je vÃ¡pnitÃ¡
ti vrchu KaliÅ¡te a Butkov.              schrÃ¡nka. Viacero nÃ¡lezov skamenelÃ­n
Asi pred 140 miliÃ³nmi rokov doÅ¡lo k

 str. 8 LZ 02 / 2018</code></pre>
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