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Geological Formation

Velabrum

Valleys

The Velabrum is a low valley in the city of Rome that connects the Forum with the Forum Boarium and the Capitoline Hill with the western slope of the Palatine Hill, though its outer boundaries are not sharply defined. Ancient writers believed the area had once been a swamp drained by the construction of the Cloaca Maxima, a claim later disproven by core samples taken from the valley in 1994, and the low ground remained prone to flooding from the Tiber even afterward, until the surrounding ground level was raised following the fire under Nero. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Connections

Caused By

Erosion, Processes

Wikidata P31 formation-type mapped to formative process Erosion via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Velabrum

In Discipline

Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Velabrum
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Velabrum
Sources
Velabrum (Wikipedia)
Lead section
Quote, Lead section
The Velabrum (Classical Latin: [weː.laː.brũ]) is the low valley in the city of Rome that connects the Forum with the Forum Boarium, and the Capitoline Hill with the western slope of the Palatine Hill.
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Wikidata: Velabrum
Wikidata Q2140194, class allow-list match (w-wdresolver-0926)View the Source
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