De Horst's population is 1,250.
Normal
Horsts and grabens are geological formations resulting from tectonic activity. A horst is an elevated block of the Earth's crust, while a graben is a depressed block between two horsts. These features commonly occur in regions experiencing extensional tectonics, such as the East African Rift Valley and the Basin and Range Province in the western United States. They are characterized by parallel mountain ranges (horsts) and valleys (grabens) formed due to the movement of tectonic plates.
The population of Lloret de Mar is 37,734.
In 2021, the population of De Kiel is 265 974
De Blesse's population is 800.
The population of De Kwakel is 3,880.
De Woude's population is 160.
De Groeve's population is 450.
De Rietschoof's population is 120.
De Goorn's population is 2,800.
The population of De Falom is 260.
De Hoeve's population is 430.