Category:Geology of South America by geochronology

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Temperate regions: North America · South America‎ · Africa · Europe · Asia · Oceania – Polar regions: Antarctica · Arctic – Other regions:

Precambrian	Phanerozoic geology of South America
Preceded by Proterozoic Eon	Phanerozoic geology of South America
	Paleozoic Era						Mesozoic Era			Cenozoic Era
	Cambrian	Ordovician	Silurian	Devonian	Carboniferous	Permian	Triassic	Jurassic	Cretaceous	Paleogene	Neogene	4ry

Subcategories

This category has the following 38 subcategories, out of 38 total.

Geology of South America by country by geochronology (35 C)
Geology of South America by era (1 C)

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A

Archean geology of South America (2 F)

C

Cambrian geology of South America (4 C, 3 F)
Carboniferous geology of South America (3 C, 2 F)
Cenozoic geology of South America (10 C, 1 F)
Cretaceous geology of South America (12 C, 12 F)

D

Devonian geology of South America (2 C)

E

Eocene geology of South America (1 C, 4 F)

G

Geology of Ecuador by geochronology (14 C)
Phanerozoic geology of South America (7 C)

H

Holocene geology of South America (3 C)

J

Jurassic geology of South America (9 C, 6 F)

M

Mesoproterozoic geology of South America (1 F)
Mesozoic geology of South America (10 C)
Miocene geology of South America (4 C, 7 F)

N

Neogene geology of South America (6 C)
Neoproterozoic geology of South America (1 C, 2 F)

O

Oligocene geology of South America (1 C)
Ordovician geology of South America (3 C, 2 F)

P

Paleocene geology of South America (2 C, 2 F)
Paleogene geology of South America (7 C)
Paleoproterozoic geology of South America (1 F)
Paleozoic geology of South America (8 C, 1 F)
Permian geology of South America (4 C, 1 F)
Pleistocene geology of South America (4 C, 4 F)
Pliocene geology of South America (3 C, 1 F)
Precambrian geology of South America (6 C, 3 F)
Proterozoic geology of South America (3 C, 3 F)

Q

Quaternary geology of South America (7 C, 2 F)

S

Silurian geology of South America (2 C, 1 F)

T

Triassic geology of South America (8 C, 7 F)

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