If you want all 24 then here they are.
Colombia
Argentina
Brazil
France
Canada
USA
Spain
Angola
UK
South Africa
Venezuela
Gabon
Cape Verde
Costa Rica
Ghana
Denmark
Uruguay
Guatemala
Portugal
Barbados
Antigua and Barbuda
Morocco
Dominican Republic
Guyana
Hope this helps :))))
Answer:
The grain size
Explanation:
The grain size can provide lot of clues for us when it comes to the formation of the rocks, the conditions in which they formed, and even what happened after their initial formation. The reason for this is that the grains vary in size and shape depending on the conditions in which the rocks formed. If the magma/lava cooled of quickly, the grains will be very small, almost unnoticeable, and that is a sign that the cooling appeared on the surface, very close to it, or in the presence of water. On the other hand, if the magma cooled slowly, the grains will be large and well defined, and that is a sign that the magma was cooling off slowly, deep into the crust, where there's higher temperature and pressure.
Europeans face greater risk of illness, property damage and job losses because of the impacts of climate change on the seas around them.
Worried citizens, whose biggest related top-of-mind concerns are sea level rise and coastal erosion, are taking personal actions to reduce carbon emissions. However, they largely blame climate change on other groups of people or nations and assign governments and industry responsibility for mitigating the problem (though they perceive government and industry as ineffective on the issue).
B native elements is the class of minerals
Granite
T: Phaneritic, Pegmatitic
P: Craton. Near Intrusive bodies such as a batholith
Plutonic
Minerals: Major: Plagioclase, K-spar
Granite #2
T: Phaneritic
P: same as above
plutonic
minerals: Major: Kspar Minor: Quartz and plag
Syenite:
T: Phaneritic
P: intrusive body. common in sills and more mafic bodies.
minerals: mainly alkali feldspar and amphibole