Their evidence comes from rocks at earths surface.
Seismic waves
physical structure is geology and geology is a movement in the earths crust which is also physical structure.
Seismic waves, generated by earthquakes or artificial sources, travel through the Earth and provide critical information about its interior structure. By analyzing the speed and behavior of these waves as they pass through different materials, scientists can infer the composition and state of the Earth's layers. For instance, seismic waves travel faster through solid materials than through liquids, helping to identify the solid inner core and the liquid outer core. This analysis has led to a greater understanding of the Earth's internal structure, including the mantle and crust.
Geologists use seismic waves to map the Earth's interior. By studying how these waves travel through the Earth, geologists can infer information about the composition and structure of different layers beneath the surface. This helps them understand the different layers of the Earth, such as the crust, mantle, and core.
Their evidence comes from rocks at earths surface.
Sun
Oceans are the greatest sources.
Seasons
Geologists gather direct evidence about Earth's interior from seismic waves, which are generated by earthquakes and can provide information about the composition and structure of the different layers beneath the surface. They also study rocks brought up from deep within the Earth's crust through volcanic eruptions or mountain building processes to understand the materials present in the interior. By analyzing these direct sources of information, geologists can create models and theories about the Earth's interior composition and processes.
the sun and the moon
Techtonic plates
geologist study the earths structure.
Seismic waves
mantle
Geology
physical structure is geology and geology is a movement in the earths crust which is also physical structure.