Room 3: The Age of the Heels (The Pleistocene)

[vc_row full_width=”stretch_row” parallax=”content-moving” css=”.vc_custom_1531741217376{background-image: url(http://museosquiroga.org/wp-content/uploads/2018/07/PREGAMENTO-XEOLÓXICO-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 3: The Age of the Heels (The Pleistocene)” 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]The action of ice glaciers during Pleistocene (geological process that started 2.58 million years ago and ended 10,000 years ago) pronounced the remains of glaciers of the Courel´s Mountains, which are interpreted considering the material remains present on the ground and the footprints left in the landscape by the action of ice.[/vc_column_text][/vc_column][/vc_row][vc_row][vc_column width=”1/6″][/vc_column][vc_column width=”2/3″][vc_gallery interval=”3″ images=”211″ img_size=”large” css_animation=”bounceInLeft”][/vc_column][vc_column width=”1/6″][/vc_column][/vc_row]