About: Eparchaean Unconformity

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Tirupati Eparchaean Unconformity, a notified National Geo-heritage Monument is a major discontinuity of stratigraphic significance that represents a period of remarkable serenity in the geological history of the earth i.e. sudden changes and discontinuity in the rock layers in earth's crust. It is seen at the steep natural slopes, road scars and ravines in the Tirupati – Tirumala Ghat road in Tirupati district of Andhra Pradesh, India.

Attributes	Values
rdf:type	yago:WikicatVillagesInChittoorDistrict geo:SpatialThing yago:GeographicalArea108574314 yago:Location100027167 yago:Object100002684 yago:PhysicalEntity100001930 yago:Region108630985 yago:YagoGeoEntity yago:YagoLegalActorGeo yago:YagoPermanentlyLocatedEntity disease yago:Settlement108672562 yago:Village108672738
rdfs:label	Eparchaean Unconformity (en)
rdfs:comment	Tirupati Eparchaean Unconformity, a notified National Geo-heritage Monument is a major discontinuity of stratigraphic significance that represents a period of remarkable serenity in the geological history of the earth i.e. sudden changes and discontinuity in the rock layers in earth's crust. It is seen at the steep natural slopes, road scars and ravines in the Tirupati – Tirumala Ghat road in Tirupati district of Andhra Pradesh, India. (en)
foaf:homepage	https://www.gsi.gov.in
name	Tirupati Eparchaean Unconformity (en)
geo:lat	13.683300 (xsd:float)
geo:long	79.349998 (xsd:float)
foaf:depiction
dcterms:subject	Geography of Tirupati district National Geological Monuments in India Tirupati Geology of Andhra Pradesh Tirupati district
Wikipage page ID	24443499 (xsd:integer)
Wikipage revision ID	1111066932 (xsd:integer)
Link from a Wikipage to another Wikipage	Precambrian Proterozoic Quartzites Geography of Tirupati district Renigunta Volcanic Peninsular Geological Survey of India Gneisses Granites Nagari, Andhra Pradesh Orogeny Andhra Pradesh Fauna Bangalore Tirumala Tirupati district National Geological Monuments in India Tirupati Eastern Ghats Palakonda Dike (geology) Flora Road Archean Chennai Tirupati Temple Geology of Andhra Pradesh South India Srikalahasti Hyderabad, Andhra Pradesh Kurnool Tirupati district Sedimentary rocks Shales Sill (geology) Tirupati (city) Dolerite Ghat Mya (unit) Stratigraphy Paleoecology Velikonda Range National Geological Monument Dyke (geology) Cudappah
Link from a Wikipage to an external page	https://www.gsi.gov.in
sameAs	Eparchaean Unconformity Eparchaean Unconformity Eparchaean Unconformity Eparchaean Unconformity
dbp:wikiPageUsesTemplate	dbt:Infobox_landform dbt:Commons_category dbt:Convert dbt:Coord dbt:Reflist dbt:Use_Indian_English dbt:Use_dmy_dates dbt:Andhra_Pradesh dbt:Tirupati_topics
thumbnail	wiki-commons:Special:FilePath/Tirupati_in_Andhra_Pradesh_(India).svg?width=300
location	Tirupati, India (en)
map caption	Location in India (en)
map image	Tirupati in Andhra Pradesh .svg (en)
website	https://www.gsi.gov.in
georss:point	13.6833 79.35
has abstract	Tirupati Eparchaean Unconformity, a notified National Geo-heritage Monument is a major discontinuity of stratigraphic significance that represents a period of remarkable serenity in the geological history of the earth i.e. sudden changes and discontinuity in the rock layers in earth's crust. It is seen at the steep natural slopes, road scars and ravines in the Tirupati – Tirumala Ghat road in Tirupati district of Andhra Pradesh, India. In 2001, the Geological Survey of India (GSI) declared the unconformity to be one of the 26 "Geological Monuments of India". GSI's commemoration document, published on the occasion of the 150 years anniversary celebration, provides an insight into the formation of the subcontinent, the orogeny, the paleoenvironment and the exotic collection of paleo-flora and fauna. The details provided for the Eparchaean Unconformity monument indicate that this feature forms the boundary surface between Proterozoic Nagari Quartzites and Archaean granite. The time gap between the formation of the two units is at least 500 Ma. At this location, the boundary is between sedimentary rocks of the Cudappah Supergroup, 1600 million years in age, and Archaean rocks comprising granites, gneisses and dolerite dykes that are more than 2100 million years old. This unconformity gives an indication of the enormous time gap in the creation of the earth's crust. (en)
gold:hypernym	Discontinuity

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