minerals inside the rock determine the rocks composition
Babe and Miss Potter are compositions by Nigel Westlake.
what compositions did maurice ravel write
Polyphonic compositions started in about the Baroque period, with Bach and Handel. Monophonic compositions-Medieval, one simple melody. Homophonic compositions-Reneissance, one melody accompanied by chords. Polyphonic compositions-Baroque, many melodies at the same time, SATB (soprano, alto, tenor, bass) compositions start.
u can find Chinese compositions at www.zwzk.com
I can't answer that because he made 626 compositions. BUT..... one of his most famous compositions of all times is the Magic Flute.
in geology
by their texture. : )
yes because they have different chemical compositions
Mafic igneous compositions have the lowest silica content, followed by ultramafic compositions. Mafic rocks are rich in magnesium and iron and have silica contents ranging from 45-52%. Ultramafic rocks have even lower silica content, typically below 45%.
Rocks with stripes are known as banded rocks or striped rocks. These stripes are often caused by the layering of different minerals or the presence of alternating bands of different mineral compositions within the rock.
The Dieke diagram is significant in geology because it helps to visualize and understand the relationships between different minerals and their compositions in rocks. It is a useful tool for geologists to interpret the origins and histories of rocks based on their mineral compositions.
The process through which single parent magma can form rocks with different compositions is known as fractional crystallization. It occurs as the magma cools and solidifies, with different minerals crystallizing at different temperatures. As these minerals crystallize and settle out of the magma, they can form different rock compositions depending on the minerals that have formed. This process can produce a range of rock compositions from a single parent magma.
When old rocks are partially melted or squeezed, they can form metamorphic rocks. Examples include gneiss, schist, and marble. These rocks exhibit new textures and compositions due to the heat and pressure they have experienced.
They are classified by the amount of silica vs the amount of alkalies are in the rocks or magma.
granitic rocks. They are typically intermediate in silica content and often contain minerals such as feldspar, amphibole, and pyroxene. Andesitic rocks are associated with volcanic activity at convergent plate boundaries.
Mafic rocks are generally denser than felsic rocks due to their higher content of iron and magnesium minerals. This higher density is attributed to the presence of heavier elements in mafic compositions.
The cooling rate of molten rock