Monday, 3 April 2023

Explaining crystal size in igneous and metamorphic rocks

The new ELI today is 'Building silicates; simulating crystal size during the cooling of magma and during recrystallisation in solid rock'.

 

This Earthlearningidea is a consolidation exercise to show how cooling/recrystallisation rates might explain crystal size in igneous and metamorphic rocks.

Related activities can be found in the categories 'Igneous processes' and 'Metamorphic processes'.

2 comments:

Earthtree said...

Earth Learning Idea makes me emotionallly;)

Anonymous said...

This earth learning idea suggests that the size of silicate tetrahedron increases in size but the distance between oxygen atoms and the central silicon atom is FIXED by atomic physics I am Sorry but this will give a completely false idea of magma crystallisation and lead to misconceptions in the future. Please alter this