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Statements

Subject Item
dbr:Intra-volcanic_sedimentary_rock_in_North_Ethiopia
rdf:type
geo:SpatialThing
rdfs:label
Intra-volcanic sedimentary rock in North Ethiopia
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.
dbp:name
Intra-volcanic sedimentary rock
geo:lat
13.65520000457764
geo:long
39.17309951782227
foaf:depiction
n13:Rock_sample_2_Interbedded_lacustrine_Meri'a_Ziban.jpg n13:Ksad_Addi_Amyuq_near_Hagere_Selam.jpg n13:Tertiary_lacustrine_deposits_at_Gumuara.jpg
dcterms:subject
dbc:Geologic_formations_of_Ethiopia
dbo:wikiPageID
61376569
dbo:wikiPageRevisionID
937593782
dbo:wikiPageWikiLink
dbr:Molluscs dbr:Interfingered dbr:Pelletoidal_wackestone dbr:Internal_moulds dbr:Isomorphic_substitution dbr:Tertiary dbr:Oligocene dbr:Ethiopian_Highlands dbr:Lanistes dbr:Ethiopia-Yemen_Continental_Flood_Basalts dbr:Diatomites dbr:Chert dbr:Tigray_Region n12:Tertiary_lacustrine_deposits_at_Gumuara.jpg dbr:Mollusc dbr:Silicified dbr:Mudstone dbr:Alaji_Basalts dbr:Ashangi_Basalts dbr:Monolithic_church dbr:Hagere_Selam_(Degua_Tembien) dbr:Lamination dbr:Geological_formation dbr:Pirenella_conica dbr:Diatomite dbr:Calcium_carbonate dbr:Gastropod dbr:Achatinidae dbr:Degua_Tembien dbr:Pila_(gastropod) n12:Rock_sample_2_Interbedded_lacustrine_Meri'a_Ziban.jpg dbc:Geologic_formations_of_Ethiopia dbr:Basalt dbr:Silicium dbr:Calcium dbr:Cherty_nodules
owl:sameAs
wikidata:Q85846181 n16:BxjL1
dbp:underlies
dbr:Alaji_Basalts
dbp:wikiPageUsesTemplate
dbt:Location_map~ dbt:Convert dbt:Coord dbt:Fossilrange dbt:Location_map+ dbt:ETH dbt:Infobox_rockunit
dbo:thumbnail
n13:Ksad_Addi_Amyuq_near_Hagere_Selam.jpg?width=300
dbp:caption
Ksad Addi Amyuq near Hagere Selam
dbp:period
Oligocene
dbp:region
dbr:Tigray_Region
dbp:type
dbr:Geological_formation
georss:point
13.6552 39.1731
dbo: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.
dbp:extent
Northern Ethiopian Highlands
dbp:namedby
:It:Giovanni Merla
dbp:otherlithology
dbr:Diatomite
dbp:overlies
dbr:Ashangi_Basalts
dbp:prilithology
dbr:Silicified dbr:Mudstone
prov:wasDerivedFrom
wikipedia-en:Intra-volcanic_sedimentary_rock_in_North_Ethiopia?oldid=937593782&ns=0
dbo:wikiPageLength
7562
foaf:isPrimaryTopicOf
wikipedia-en:Intra-volcanic_sedimentary_rock_in_North_Ethiopia
geo:geometry
POINT(39.173099517822 13.655200004578)