Vergilov Ridge Explained

Vergilov Ridge (Bulgarian: Вергилов хребет, 'Vergilov Hrebet' \ver-'gi-lov 'hre-bet\) is a submarine ridge in South Bay, Livingston Island in the South Shetland Islands, Antarctica. It extends 3.5 km in a southeast-northwest direction between the Vergilov Rocks and the opposite Pimpirev Beach at a depth of over 50 m, with depths exceeding 100 m on both sides of the ridge. It was formed as a frontal moraine of Perunika Glacier between the 13th and 17th centuries.

The feature takes its name from the Vergilov Rocks.

Location

Vergilov Ridge is centred at -62.63°N -60.3931°W. Spanish mapping in 1991.

Isla Livingston: Península Hurd. Mapa topográfico de escala 1:25000. Madrid: Servicio Geográfico del Ejército, 1991. (Map reproduced on p. 16 of the linked work)
L.L. Ivanov. Antarctica: Livingston Island and Greenwich, Robert, Snow and Smith Islands. Scale 1:120000 topographic map. Troyan: Manfred Wörner Foundation, 2009.
Antarctica, South Shetland Islands, Livingston Island: Bulgarian Antarctic Base. Sheets 1 and 2. Scale 1:2000 topographic map. Geodesy, Cartography and Cadastre Agency, 2016. (in Bulgarian)
Antarctic Digital Database (ADD). Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR). Since 1993, regularly upgraded and updated.
L.L. Ivanov. Antarctica: Livingston Island and Smith Island. Scale 1:100000 topographic map. Manfred Wörner Foundation, 2017.