Peruvian flat-slab segment: Difference between revisions
Content deleted Content added
No edit summary |
redir unsourced stub |
||
| (3 intermediate revisions by one other user not shown) | |||
| Line 1: | Line 1: | ||
#Redirect [[Andean Volcanic Belt#Volcanic gaps]] |
|||
{{Unreferenced|date=June 2009}} |
|||
The '''Peruvian flat-slab segment''' is a region, spanning the latitudes of 3°–15°, were the [[subduction]] angle of the [[Nazca Plate]] is relatively low causing the absence of [[volcanism]] in the [[Andes]]. This volcanic gap is located south of the [[North Volcanic Zone]] and north of the [[Central Volcanic Zone]]. It is believed that the [[subduction]] of the [[Nazca Ridge]] is causing this gap in volcanic activity due to a decrease in the subduction angle. |
|||
[[Category:Geology of Peru]] |
|||
[[Category:Plate tectonics]] |
|||
{{tectonics-stub}} |
|||
{{chile-geo-stub}} |
|||
Latest revision as of 21:07, 2 June 2010
Redirect to: