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Extrusive Rocks

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Extrusive Rocks 

(or effusive rocks), igneous rocks which, like modern lavas, poured out onto the surface of the earth through volcanic vents or cracks in the earth’s crust and solidified in the form of flows, sheets, and domes.



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The term was used initially to designate serpentinite and later on, a suite of mafic and ultramafic intrusive rocks (ultramafic rocks, gabbro, and diabase) and volcanic extrusive rocks (Brongniart 1821).
Redton initially focused on the area because it displayed a concentration of high gold values that corresponded with alkali intrusive and extrusive rocks.
Geologically, the project area is a 15 million year old volcanic eruptive center dominated by a bi-modal suite of flow domes, dikes, and extrusive rocks that were intensively and extensively altered and mineralized by a hydrothermal system of the same age.
 
 
 
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