Difference between revisions 2488451 and 2490221 on glwikiSon afloramentos rochosos que polo xeral se orixinan cando se descobren antigas fendas, denominadas [[diáclases]]. Atravesan a [[rocha]] na que se aloxan, que é denominada [[rocha de encaixe]]. [[Categoría:Xeoloxía]] [[af:Dyk]] [[az:Damba]]⏎ [[be:Дамба]] [[be-x-old:Дамба]] [[bg:Дига]] [[br:Chaoser]] [[ca:Dic]] [[cs:Hráz (stavba)]] [[da:Dige]] [[de:Deich]] [[en:Levee]] [[eo:Digo]] [[es:Dique]] [[et:Tamm (ehitis)]] [[fr:Digue]] [[fy:Dyk]] [[he:סוללה (הנדסה אזרחית)]] [[ia:Dica]] [[io:Digo]] [[it:Argine]] [[ja:堤防]] [[kk:Дамба]] [[ko:제방]] [[lb:Däich]] [[lv:Dambis]] [[nds:Diek (Bowark)]] [[nl:Dijk (waterkering)]] [[nn:Dike]] [[no:Dike]] [[pl:Grobla]] [[pt:Dique]] [[ro:Dig]] [[ru:Дамба]] [[sk:Hrádza (stavba)]] [[sq:Diga]] [[sv:Vall (anläggning)]] [[th:คันดินธรรมชาติ]] [[uk:Дамба]] [[vec:Àrzere]] [[vi:Đê]] All content in the above text box is licensed under the Creative Commons Attribution-ShareAlike license Version 4 and was originally sourced from https://gl.wikipedia.org/w/index.php?diff=prev&oldid=2490221.
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