Značilnosti mikro psevdokraških oblik na območju blatnega vulkana Pâclele Mari (Romunija)
DOI:
https://doi.org/10.3986/ac.v53i1.13549Ključne besede:
pseudokarst, badland, piping, mud tubes, Păclele Mare mud volcanos, Buzău Geopark RomaniaPovzetek
V članku predstavljamo rezultate geomorfološke študije mikro psevdokraških oblik, ki so nastale na območju blatnih vulkanov Pâclele Mari, ki je del znanega območja blatnih vulkanov Berca-Arbănași v okrožju Buzău v podkarpatski regiji, Romunija. Na proučevanem območju je mogoče opaziti različne vrste psevdokraških votlin, zlasti na nagnjenem obrobju območja blatnih vulkanov, kjer so nastala erozijska žarišča (psevdokras erozijskih žarišč), in na blatnih tokovih, kjer se je razvil reogeni psevdokras. Na površini blatnega plazu, ki teče v koritu, se blato zgošča in naguba, pri premikanju se blato kopiči, nato pa zapolni jarek tekočega blata. Ti zapolnjeni jarki mikro velikosti so podobno oblikovani kot lavine cevi v tokovih lave na območjih pravih vulkanov. Za dopolnitev terenskih meritev smo opravili raziskave s kvadrokopterji DJI Phantom 3 in 4 ter Mavic Pro, da bi določili reliefne oblike za fotogrametrijo. Na vzorcih sedimentov, odvzetih na območju blatnih vulkanov, so bili opravljeni testi zrnate sestave z analizatorjem laserske difrakcije delcev.
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