Evidence supporting the idea that Earth's core is composed of an iron-nickel alloy includes seismic studies showing that the outer core is liquid and has lower density than the inner core, which is solid and denser. Additionally, the Earth's magnetic field, generated by the movement of molten iron and nickel in the outer core, aligns with this composition. During Earth's formation, heavier elements like iron and nickel sank to the center due to their high density, a process known as planetary differentiation, which resulted in the formation of the core.
Their evidence comes from rocks at earths surface.
magnetic rocks on the ocean floor show that the Earths magnetic field has been frequently reversed forming new sea floor.
The lithosphere.
Seismic waves
This is where the weaknesses in the earths crust lie and it is the easiest place for lava to spew out of these weaker areas, therefore forming volcanoes
At convergent boundaries some mantle material can melt and rise through the crust, forming volcanoes.
Their evidence comes from rocks at earths surface.
magnetic rocks on the ocean floor show that the Earths magnetic field has been frequently reversed forming new sea floor.
Seasons
The lithosphere.
The gravitational forces of the Sun and Moon, effect the earths oceans by forming tides.
Diamond is the earths hardest material.
How do changes in heat energy affect the density of earths mantle material
Seismic waves
Magma
a. seismic waves b. volcanoes c. earthquakes d. rocks
Rock samples