Geology of Equatorial Guinea
The geological basement of the central and eastern regions Equatorial Guinea is composed of Precambrian rocks which form a part of the Congo craton. They include gneiss, greenstone, schist-amphibolite and granitoids. These older rocks are overlain by sedimentary rocks of Mesozoic, Neogene and Quaternary age in the west and along the coast. The islands of Pagalu and Bioko (Annobon and Fernando Poo) are of relatively recent volcanic origin, forming a part of the Cameroon Volcanic Line.
Link from a Wikipage to another Wikipage
primaryTopic
Geology of Equatorial Guinea
The geological basement of the central and eastern regions Equatorial Guinea is composed of Precambrian rocks which form a part of the Congo craton. They include gneiss, greenstone, schist-amphibolite and granitoids. These older rocks are overlain by sedimentary rocks of Mesozoic, Neogene and Quaternary age in the west and along the coast. The islands of Pagalu and Bioko (Annobon and Fernando Poo) are of relatively recent volcanic origin, forming a part of the Cameroon Volcanic Line.
has abstract
The geological basement of the ...... of the Cameroon Volcanic Line.
@en
Wikipage page ID
39,100,405
page length (characters) of wiki page
Wikipage revision ID
963,173,595
Link from a Wikipage to another Wikipage
wikiPageUsesTemplate
comment
The geological basement of the ...... of the Cameroon Volcanic Line.
@en
label
Geology of Equatorial Guinea
@en