Milne Land project is located in the eastern part of Milne Land and is formed from both Caledonian Crystalline and Mesozoic marine sediments and Tertiary volcanic rocks. There is a significant occurrence of rare earth elements on this license.

Milne Land is one of the islands in an extensive fjord system characteristic of the central area of East Greenland. Its morphology is quite rugged, with altitudes ranging from 0 to above 2100 masl. The western part of Milne Land has the most distinctive morphology composed from Caledonian Crystalline complex. The non-glaciated eastern part of Milne Land, with altitudes between 0 – 1000 masl, formed from Mesozoic sediments, in addition to the Caledonian Crystalline, already has a substantially milder morphology. Since Milne Land is already far above the Arctic Circle, during the annual cycle there is a characteristic alternation of polar day and polar night. Milne Land is easily accessible both by air and sea transport.

Milne Land is one of the islands in an extensive fjord system characteristic of the central area of East Greenland. Its morphology is quite rugged, with altitudes ranging from 0 to above 2100 masl. The western part of Milne Land has the most distinctive morphology composed from Caledonian Crystalline complex. The non-glaciated eastern part of Milne Land, with altitudes between 0 – 1000 masl, formed from Mesozoic sediments, in addition to the Caledonian Crystalline, already has a substantially milder morphology. Since Milne Land is already far above the Arctic Circle, during the annual cycle there is a characteristic alternation of polar day and polar night. Milne Land is easily accessible both by air and sea transport.

The project is in an advanced stage. Final drilling works and feasibility study are being prepared in the following project period.