The main conclusions were that about 60% of the research area was affected by erosion and that approximately 54% of the eroded areas are sources of aeolian materials.
Helstu niðurstöður voru þær að jarðvegsrof reyndist vera á um 60% rannsóknarsvæðisins og af heildarstærð gróðursnauðs lands reyndust tæp 54% þess vera uppsprettusvæði fyrir áfoksefni.