Earth:Marichuela Formation

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Short description: Geological formation in the Colombian Andes
Marichuela Formation
Stratigraphic range: Late Miocene-Early Pliocene
~8.2–5 Ma
TypeGeological formation
UnderliesTilatá Formation
OverliesGuadalupe Group
Thicknessup to 40 metres (130 ft)
Lithology
PrimaryConglomerate
Location
Coordinates [ ⚑ ] : 4°21′40.3″N 74°07′50″W / 4.361194°N 74.13056°W / 4.361194; -74.13056
RegionBogotá savanna, Altiplano Cundiboyacense
Eastern Ranges, Andes
Country Colombia
Type section
Named forMarichuela neighbourhood
Named byHelmens & Hammen
LocationUsme, Bogotá
Year defined1995
Coordinates [ ⚑ ] 4°21′40.3″N 74°07′50″W / 4.361194°N 74.13056°W / 4.361194; -74.13056
RegionCundinamarca
Country Colombia

The Marichuela Formation (Spanish: Formación Marichuela, N1m) is a geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists of coarse to very coarse conglomerates. The Marichuela Formation dates to the Neogene period; Late Miocene to Early Pliocene epochs, and has a maximum thickness of 40 metres (130 ft).

Etymology

The formation was defined by Helmens and Van der Hammen in 1995 and named after the Marichuela neighbourhood of Usme.[1] Part of the Marichuela Formation had been included in the Conos de Tunjuelo, defined by Julivert in 1961.[2]

Description

Lithologies

The Marichuela Formation consists of coarse to very coarse conglomerates.[1]

Stratigraphy and depositional environment

The Marichuela Formation unconformably overlies the Cretaceous rocks of the Guadalupe Group. The age has been estimated to be Late Miocene to Early Pliocene.[3] The depositional environment has been interpreted as alluvial fans, caused by earthquakes or heavy rains.[4]

Outcrops

Lua error in Module:Location_map at line 522: Unable to find the specified location map definition: "Module:Location map/data/Bogotá savanna" does not exist. The Marichuela Formation is apart from its type locality in the Usme Synclinal, the valley of the Tunjuelo River, found in the synclinals of Neusa, Sisga and La Calera.[1]

Regional correlations

See also

Good article nominee Geology of the Eastern Hills
B-Class article Geology of the Ocetá Páramo
C-Class article Geology of the Altiplano Cundiboyacense

Notes

References

  1. 1.0 1.1 1.2 Montoya & Reyes, 2005, p.65
  2. Suna Hisca, s.a., p.45
  3. Montoya & Reyes, 2005, p.67
  4. Montoya & Reyes, 2005, p.66

Bibliography

  • Montoya Arenas, Diana María, and Germán Alfonso Reyes Torres. 2005. Geología de la Sabana de Bogotá, 1–104. INGEOMINAS.
  • N., N. s.a. Parque Ecológico Distrital de Montaña Entrenubes – Tomo I – Componente Biofísico – Geología, 36–51. Corporación Suna Hisca.

Maps

External links