When I was first interested in the internal structure and composition of the Earth in 1968, all we had were seismic data, experimental work on silicate melts and the rocks on the Earth's surface. The models were essential built on that data, throwing in some meteorite data and what we knew of astrophysical phenomena. By melting a basalt, we can approximate what the temperature of a basaltic magma could be. Nucleosynthesis, BBN and from supernovae gave insights into what the general composition of the Earth is likely to be. Seismic, magnetic and gravity data refined the model. 15 years later Sunoco bought into seismic programs intended to study the core. I justified that expense because it also revealed crustal information. Today, geophysical techniques are defining the structure in greater detail. Diamond anvil cell studies have totally opened the possible scenarios for composition and structure of the inner earth. Data from those studies give us possible composition of rocks and minerals, as well as melting and cooling temperatures and pressures.