{"id":1007,"date":"2016-02-03T17:14:32","date_gmt":"2016-02-03T15:14:32","guid":{"rendered":"http:\/\/archeol.sav.sk\/?page_id=1007"},"modified":"2016-02-24T21:02:44","modified_gmt":"2016-02-24T19:02:44","slug":"liptovska-sielnica-liptovska-mara-okr-liptovsky-mikulas","status":"publish","type":"page","link":"https:\/\/archeol.sav.sk\/index.php\/sk\/liptovska-sielnica-liptovska-mara-okr-liptovsky-mikulas\/","title":{"rendered":"Liptovsk\u00e1 Sielnica-Liptovsk\u00e1 Mara (okr. Liptovsk\u00fd Mikul\u00e1\u0161)"},"content":{"rendered":"

Poloha I\/\u201eHavr\u00e1nok\u201c<\/p>\n

\u00a0<\/em>Realiz\u00e1cia v\u00fdskumu: ved\u00faca v\u00fdskumu: Mgr. Lucia Benedikov\u00e1, PhD.<\/p>\n

Odborn\u00e1 spolupr\u00e1ca: Mgr. Miriam \u0160vihurov\u00e1, PhDr. Karol Pieta, DrSc.<\/p>\n

Rok v\u00fdskumu: 2015<\/p>\n

Druh v\u00fdskumu: rev\u00edzny, pre vedeck\u00e9 a dokumenta\u010dn\u00e9 \u00fa\u010dely<\/p>\n

Druh n\u00e1leziska: fortifik\u00e1cia<\/p>\n

Datovanie: stredn\u00e1 a\u017e neskor\u00e1 doba lat\u00e9nska<\/p>\n

 <\/p>\n

\"LiptMara2<\/a>
Liptovsk\u00e1 Mara \u2013 Havr\u00e1nok (Foto: K. Pieta)<\/figcaption><\/figure>\n

Rev\u00edzny v\u00fdskum sa uskuto\u010dnil v\u00a0juhoz\u00e1padnom segmente neskorolat\u00e9nskeho valu na Havr\u00e1nku, ktor\u00fd sa sk\u00famal v\u00a0rokoch 1965 \u2013 1966 v\u00a0r\u00e1mci sondy III (K. Pieta; predbe\u017en\u00e1 publik\u00e1cia p. Archeologick\u00e9 rozhledy XIX, 1967, 618 \u2013 620, 624 \u2013 631). Cie\u013eom bolo overenie stratigrafie a vyzdvihnutie vzoriek z vrstvy zuho\u013enaten\u00fdch rastlinn\u00fdch makrozvy\u0161kov, ktor\u00e1 mala pod\u013ea p\u00f4vodnej interpret\u00e1cie patri\u0165 najstar\u0161iemu horizontu os\u00eddlenia na lokalite (tzv. vrstva pod valom; p. aj K. Pieta 1982: Die P\u00fachov Kultur. Nitra, Taf. XXVII: 13-27), pre potreby datovania C14.<\/p>\n

V\u00fdskum sa realizoval v\u00a0r\u00e1mci projektu APVV-14-0842 ako jedna z\u00a0viacer\u00fdch analogicky zameran\u00fdch ter\u00e9nnych aktiv\u00edt v\u00a0regi\u00f3ne Liptova v\u00a0roku 2015 (p. Dem\u00e4novsk\u00e1 Dolina, Z\u00e1va\u017en\u00e1 Poruba), ktor\u00fdch spolo\u010dn\u00fdm cie\u013eom bolo z\u00edskanie dostato\u010dn\u00e9ho mno\u017estva prame\u0148ov d\u00f4le\u017eit\u00fdch pre poznanie neskorohal\u0161tatsk\u00e9ho a\u017e stredolat\u00e9nskeho os\u00eddlenia Liptova.<\/p>\n

Po odstr\u00e1nen\u00ed n\u00e1letovej zelene sa za\u010distil severn\u00fd profil b\u00fdvalej sondy III v\u00a0d\u013a\u017eke 4 m, do max. h\u013abky 2,8 m, v\u00a0ktorej bolo dosiahnut\u00e9 podlo\u017eie. Podarilo sa dolo\u017ei\u0165 dve f\u00e1zy existencie valu (obidve pravdepodobne s\u00a0prestavbami) \u2013 horn\u00fa neskorolat\u00e9nsku \u2013 pod\u013ea keramiky sk\u00f4r z\u00a0druhej polovice neskorej doby lat\u00e9nskej (mo\u017eno star\u0161ia vrstva tejto f\u00e1zy sa bude da\u0165 datova\u0165 aj sk\u00f4r \u2013 v\u0161etka keramika v\u0161ak nebola zatia\u013e preveren\u00e1), spodn\u00fa zatia\u013e nedatovan\u00fa, so zvy\u0161kami mohutnej kamennej kon\u0161trukcie z\u00a0ve\u013ek\u00fdch pieskovcov\u00fdch platn\u00ed, ktor\u00fa \u010diasto\u010dne prekr\u00fdvala a\u00a0\u010diasto\u010dne sa nach\u00e1dzala v\u00a0jej vn\u00fatri zrete\u013en\u00e1 a\u00a0pomerne hrub\u00e1 vrstva prep\u00e1len\u00fdch rastlinn\u00fdch makrozvy\u0161kov (miestami s\u00a0mocnos\u0165ou okolo 40 cm). Keramika z\u00a0tejto f\u00e1zy valu je, \u017eia\u013e, atypick\u00e1, preto sa bude da\u0165 pri chronol\u00f3gii opiera\u0165 v\u00fdlu\u010dne o\u00a0v\u00fdsledky C14 anal\u00fdz (st\u00e1le teda m\u00f4\u017ee \u00eds\u0165 aj o\u00a0star\u0161iu f\u00e1zu v\u00a0r\u00e1mci neskorej doby lat\u00e9nskej). Zo v\u0161etk\u00fdch kontextov a\u00a0vrstiev v\u00a0r\u00e1mci sk\u00famanej plochy boli systematicky odoberan\u00e9 archeobotanick\u00e9 vzorky (a, prirodzene, v\u0161etok archeologick\u00fd a\u00a0archeozoologick\u00fd materi\u00e1l; 47 pr\u00edrastkov\u00fdch \u010d\u00edsel keramiky, 63 pr\u00edrastkov\u00fdch \u010d\u00edsel rastlinn\u00fdch makrozvy\u0161kov, 14 pr\u00edrastkov\u00fdch \u010d\u00edsel kost\u00ed, 1 drobn\u00fd predmet), v\u00a0ktor\u00fdch sa makroskopicky daj\u00fa zisti\u0165 ve\u013ek\u00e9 koncentr\u00e1cie obiln\u00edn, s\u00a0men\u0161ou pr\u00edmesou strukov\u00edn (dalo by sa poveda\u0165, \u017ee jednotliv\u00e9 vzorky ani neobsahuj\u00fa hlinu, ale \u010dist\u00fd rastlinn\u00fd materi\u00e1l).<\/p>\n

\"NajmladsiClenTimu\"<\/a>
Najmlad\u0161\u00ed \u010dlen t\u00edmu (Foto: L. Benedikov\u00e1)<\/figcaption><\/figure>\n

U\u017e zo stratigrafick\u00fdch pozorovan\u00ed je zrejm\u00e9, \u017ee mohutn\u00e1 vrstva zuho\u013enaten\u00fdch rastlinn\u00fdch makrozvy\u0161kov sa nenach\u00e1dza pod valom, ako to bolo prezentovan\u00e9 po v\u00fdskume v\u00a0rokoch 1965 \u2013 1966. V\u00a0zhode s\u00a0p\u00f4vodnom interpret\u00e1ciou v\u0161ak zrejme predstavuje s\u00fa\u010das\u0165 najstar\u0161ieho horizontu archeologick\u00fdch prame\u0148ov na tomto mieste Havr\u00e1nka, t. j. star\u0161ej f\u00e1zy juhoz\u00e1padnej \u010dasti valov\u00e9ho opevnenia. K\u013e\u00fa\u010dov\u00e9 v\u00fdsledky v\u00fdskumu \u2013 fakty pre absol\u00fatnu chronol\u00f3giu doby lat\u00e9nskej \u2013 prines\u00fa a\u017e v\u00a0najbli\u017e\u0161ej bud\u00facnosti pl\u00e1novan\u00e9 C14 anal\u00fdzy z\u00edskan\u00e9ho materi\u00e1lu. Jedn\u00fdm z\u00a0cie\u013eov v\u00fdskumu bolo z\u00edska\u0165 pramene pre korel\u00e1ciu relat\u00edvnej a\u00a0absol\u00fatnej chronol\u00f3gie, \u010do sa v\u0161ak, \u017eia\u013e, vzh\u013eadom na atypick\u00fa keramiku zo spodnej vrstvy valu, nepodarilo. Pri stanovovan\u00ed vedeck\u00fdch cie\u013eov ter\u00e9nneho v\u00fdskumu v\u0161ak, samozrejme, nie je mo\u017en\u00e9 predv\u00edda\u0165, ak\u00fd charakter bude ma\u0165 z\u00edskan\u00fd archeologick\u00fd materi\u00e1l.<\/p>\n

 <\/p>\n","protected":false},"excerpt":{"rendered":"

Poloha I\/\u201eHavr\u00e1nok\u201c \u00a0Realiz\u00e1cia v\u00fdskumu: ved\u00faca v\u00fdskumu: Mgr. Lucia Benedikov\u00e1, PhD. Odborn\u00e1 spolupr\u00e1ca: Mgr. Miriam \u0160vihurov\u00e1, PhDr. Karol Pieta, DrSc. Rok v\u00fdskumu: 2015 Druh v\u00fdskumu: rev\u00edzny, pre vedeck\u00e9 a dokumenta\u010dn\u00e9 \u00fa\u010dely Druh n\u00e1leziska: fortifik\u00e1cia Datovanie: stredn\u00e1 a\u017e neskor\u00e1 doba lat\u00e9nska   Rev\u00edzny v\u00fdskum sa uskuto\u010dnil v\u00a0juhoz\u00e1padnom segmente neskorolat\u00e9nskeho valu na Havr\u00e1nku, ktor\u00fd sa sk\u00famal v\u00a0rokoch 1965 … \u010c\u00edtajte viac<\/a><\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":[],"_links":{"self":[{"href":"https:\/\/archeol.sav.sk\/index.php\/wp-json\/wp\/v2\/pages\/1007"}],"collection":[{"href":"https:\/\/archeol.sav.sk\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/archeol.sav.sk\/index.php\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/archeol.sav.sk\/index.php\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/archeol.sav.sk\/index.php\/wp-json\/wp\/v2\/comments?post=1007"}],"version-history":[{"count":5,"href":"https:\/\/archeol.sav.sk\/index.php\/wp-json\/wp\/v2\/pages\/1007\/revisions"}],"predecessor-version":[{"id":1050,"href":"https:\/\/archeol.sav.sk\/index.php\/wp-json\/wp\/v2\/pages\/1007\/revisions\/1050"}],"wp:attachment":[{"href":"https:\/\/archeol.sav.sk\/index.php\/wp-json\/wp\/v2\/media?parent=1007"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}