jordlederkontinuitet
Jordlederkontinuitet is the Norwegian term for "earth crust continuity". This concept refers to the idea that the Earth's crust is a continuous, coherent body that spans the globe.
The theory of jordlederkontinuitet was first proposed by Norwegian geologist A. E. Nordenskjöld in the late
According to this concept, the Earth's crust is not a collection of separate plates or fragments, but
The theory of jordlederkontinuitet has been influential in the development of modern plate tectonics. While it
Research on jordlederkontinuitet has also shed light on the dynamics of the Earth's crust and the processes