hovedøkten
Hovedøkten was a distinct geological formation in Oslo, Norway, which stretched from the city center to the nearby hills of the eastern part of the town, making it a topographical feature that influenced the city's layout. As the name suggests, "Hovedøkten" translates to "Main Contour" or "Main Ridge" in Norwegian, reflecting its prominent and defining characteristic in the landscape.
The formation was composed of a series of ridges and hills, primarily made up of granite, which
As the city expanded, the Hovedøkten began to disappear due to urban development and the construction of
Throughout its relatively short existence, the Hvedøkten had significant impacts on Oslo's layout and development. Its