Changes

[[File:Trinidad (Kuba) 03.jpg|thumb|Trinidad (Kuba) 03: released in the GFDL by [http://commons.wikimedia.org/wiki/User:Dino1948 Dieter Mueller].]]

[[File:Trinidad (Kuba) 03.jpg|thumb|Trinidad (Kuba) 03: released in the GFDL by [http://commons.wikimedia.org/wiki/User:Dino1948 Dieter Mueller].]]

The geology of Cuba has been a challenge to geologists because of features such as the presence of well-preserved [[Jurassic]] [[ammonite]]s, the rich [[Tertiary]] [[foraminiferal]] faunas (including remarkable [[Paleogene]] [[orbitoids]]), the gigantic Upper [[Cretaceous]] [[rudistids]], the spectacular limestone Mogotes of Pinar del Rio, the extensive outcrops of [https://wwwf.imperial.ac.uk/earthscienceandengineering/rocklibrary/viewglossrecord.php?gID=00000000012 ultrabasic] [[igneous]] rocks, the [[chromite]] and [[manganese]] deposits, and the extraordinary structural complexity. In addition to these features, the numerous petroleum seeps, many of them coming out of [[http://en.wikipedia.org/wiki/Basic_rock|basic]] igneous rock, have attracted much attention.

The geology of Cuba has been a challenge to geologists because of features such as the presence of well-preserved [[Jurassic]] [[ammonite]]s, the rich [[Tertiary]] [[foraminiferal]] faunas (including remarkable [[Paleogene]] [[orbitoids]]), the gigantic Upper [[Cretaceous]] [[rudistids]], the spectacular limestone Mogotes of Pinar del Rio, the extensive outcrops of [https://wwwf.imperial.ac.uk/earthscienceandengineering/rocklibrary/viewglossrecord.php?gID=00000000012 ultrabasic] [[igneous]] rocks, the [[chromite]] and [[manganese]] deposits, and the extraordinary structural complexity. In addition to these features, the numerous petroleum seeps, many of them coming out of [[Wikipedia:Basic_rock|basic]] igneous rock, have attracted much attention.

==Regional setting==

==Regional setting==