About: Intra-volcanic sedimentary rock in North Ethiopia     Goto   Sponge   NotDistinct   Permalink

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Between 29 and 27 million years ago, the extrusion of Ethiopia’s flood basalts was interrupted and deposition of continental sediments occurred. Inter-trappean beds outcrop in many places of the Ethiopian highlands. They consist of fluvio-lacustrine deposits, that are generally a few tens of metres thick. Often, these interbedded fluvio-lacustrine deposits are very visible because their bright colours strongly contrast with the basalt environment.

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  • Intra-volcanic sedimentary rock in North Ethiopia (en)
rdfs:comment
  • Between 29 and 27 million years ago, the extrusion of Ethiopia’s flood basalts was interrupted and deposition of continental sediments occurred. Inter-trappean beds outcrop in many places of the Ethiopian highlands. They consist of fluvio-lacustrine deposits, that are generally a few tens of metres thick. Often, these interbedded fluvio-lacustrine deposits are very visible because their bright colours strongly contrast with the basalt environment. (en)
name
  • Intra-volcanic sedimentary rock (en)
geo:lat
geo:long
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/Ksad_Addi_Amyuq_near_Hagere_Selam.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Rock_sample_2_Interbedded_lacustrine_Meri'a_Ziban.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Tertiary_lacustrine_deposits_at_Gumuara.jpg
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Wikipage page ID
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underlies
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thumbnail
caption
  • Ksad Addi Amyuq near Hagere Selam (en)
period
  • Oligocene (en)
region
type
georss:point
  • 13.6552 39.1731
has abstract
  • Between 29 and 27 million years ago, the extrusion of Ethiopia’s flood basalts was interrupted and deposition of continental sediments occurred. Inter-trappean beds outcrop in many places of the Ethiopian highlands. They consist of fluvio-lacustrine deposits, that are generally a few tens of metres thick. Often, these interbedded fluvio-lacustrine deposits are very visible because their bright colours strongly contrast with the basalt environment. (en)
extent
  • Northern Ethiopian Highlands (en)
namedby
  • :It:Giovanni Merla (en)
otherlithology
overlies
prilithology
prov:wasDerivedFrom
page length (characters) of wiki page
foaf:isPrimaryTopicOf
geo:geometry
  • POINT(39.173099517822 13.655200004578)
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