Room 1: The formation of Territory of Galicia

[vc_row full_width=”stretch_row” parallax=”content-moving” css=”.vc_custom_1531740526191{background-image: url(ÓXICO-DE-CAMPODOLA-LEIXAZOS.jpg?id=202) !important;}”][vc_column][like_sc_empty_space height_xl=”344px” height_lg=”” height_md=”” height_sm=”” height_ms=”32px” height_xs=”” id=”” class=”” css=””][/vc_column][/vc_row][vc_row][vc_column][like_sc_header type=”h3″ subheader=”Museo Xeolóxico” header=”Room 1: The formation of Territory of Galicia” bgheader=”” style=”default” color=”main” subcolor=”black” align=”left” size=”default” sr=”default” image=”” icon_type=”hidden” icon_bg=”transparent” size_px=”” use_theme_fonts=”yes” google_fonts=”” id=”” class=”” css=””][vc_column_text]Analysis of the Campodola-Leixazós folding (sinclinal of Courel), one of the most important geological events that define the territory of Galicia as we know it. How and when was it formed, and what is a folding? What types of folds exist? etc.  This room contents a collection with 32 minerals and 17 rocks from the region of Quiroga and its surroundings.[/vc_column_text][vc_gallery type=”image_grid” images=”205″ img_size=”full” css_animation=”bounceInLeft”][/vc_column][/vc_row]