The internal structure and composition of the Earth are primarily understood through seismic data, mathematical models, and experimental studies. Seismic waves, particularly body waves, provide insights into whether materials are in solid or liquid states, while advancements in geophysical techniques have refined our understanding of the Earth's layers. The use of diamond anvil cell studies has significantly contributed to determining the composition and conditions of the Earth's interior, revealing that the Earth's core is hotter than previously thought. Models of the Earth's structure are continuously updated as new data and techniques emerge, such as seismic tomography, which allows for 3-D imaging of the Earth's interior. The physical properties of deep Earth materials are influenced more by volume than pressure, and ongoing research includes studying electron spin in iron to further understand these properties. Overall, the integration of various scientific methods has enhanced our knowledge of the Earth's internal dynamics and composition.