The heart of continents is their cratons, which are the most ancient and stable parts of the Earth's crust. In the cratons are all the rare elements needed for electronic equipment. They were swept up as the Sun moved through areas where supernovae had exploded. The rare elements we need were all got indirectly from supernovae explosions. The Sun's energy comes from turning hydrogen into helium..
There are some islands which do have rare elements, and that is a sign that they were once part of a large supercontinent. So Great Britain was once part of a supercontinent. The oldest rocks are 2,700 million years old, and include many rare elements only found in cratons. Britain is a snapped-off piece of the Old Red Sandstone continent, now known as Laurasia.
Other islands that were formed from the ocean floor, as Japan, and Hawaii were, lack most of the rare elements. Japan has for many years since WWII imported iron ore from Australia. Its seizing of Manchukuo (~Manchuria) and the infamous attack on Pearl Harbour no doubt had many reasons. Lack of raw materials was one of these 
Big islands[change | change source]
In Europe[change | change source]
- Great Britain 218,995 km²
- Iceland 101,826 km²
- Ireland 81,638 km²
- The island in the north of Novaja Zemlja 47,079 km²
- Spitsbergen 38,981 km²
- The island in the south of Novaja Zemlja 33,246 km²
- Sicily 25,662 km²
- Sardinia 23,812 km²
- Nordaustlandet (archipelago of Svalbard, Norway) 14,247 km²
- Cyprus 9,234
- Corsica 8,741 km²
Other places[change | change source]
- Greenland 2,130,800 km²
- New Guinea 785,753 km²
- Borneo 748,138 km²
- Madagascar 587,041 km²
- Baffin 507,451 km²
- Sumatra 677,658 km²
References[change | change source]
- Society, National Geographic (2012-08-27). "island". National Geographic Society. Retrieved 2020-12-07.
- Toghill, Peter 2000. The geology of Britain: an introduction. Shrewsbury: Swan Hill Press. ISBN 1-85310-890-1
- Yamamuro, Shin'ichi. 2006. Manchuria under Japanese dominion. U. of Pennsylvania Press.