Both Radioactive dating of rocks retrieved from the world and Comparing cratering rates on one world to those on another.
Geologists can find the relative age of impact craters on a world because
the ones on top must be younger.
Scientists know the history of Earth's magnetic field because the magnetic field gets frozen into rocks, and plate tectonics spreads them out.
Hope it helps
Answer:
você deve começar encontrando a diferença de longitude ou graus dos dois lugares. você faz isso somando os dois números. então, divida pelos 15 ° que ocorrem em 1 hora e isso lhe dará a diferença de tempo entre dois locais na linha de data internacional.
Explanation:
espero que isso tenha ajudado Mark BRAINLIEST !!!
Mountain Peaks and Plautaeu
increases by 1 every time
Answer:
Through infrared radiation
