The Kronborg Glacier is a non-surge type valley glacier that does not drain the Greenland ice sheet directly, but flows partly from it across mountainous areas in a roughly north/south direction.
It separates the Ejnar Mikkelsen Range in the west from the Borgtinderne in the east.
Further south it separates the Watkins Range and the Lilloise Range in the west from the Wiedemann Range in the east,  until its terminus at the head of the Ravn Fjord in the East Greenland coast.

A fast-flowing glacier, it is similar in structure to the neighbouring Christian IV Glacier.
The Rosenborg Glacier is a smaller glacier flowing between both.
The Kronborg Glacier is a non-surge type valley glacier that does not drain the Greenland ice sheet directly, but flows partly from it across mountainous areas in a roughly north/south direction. It separates the Ejnar Mikkelsen Range in the west from the Borgtinderne in the east. Further south it separates the Watkins Range and the Lilloise Range in the west from the Wiedemann Range in the east,  until its terminus at the head of the Ravn Fjord in the East Greenland coast.
A fast-flowing glacier, it is similar in structure to the neighbouring Christian IV Glacier. The Rosenborg Glacier is a smaller glacier flowing between both.
Kronborg Glacier