Q1972Inge Lehmann's 1936 analysis of earthquake waves showed that Earth's core contains a solid inner core inside its liquid outer region.
Seismologists expected certain earthquake waves to vanish in the shadow made by Earth's liquid core, yet instruments recorded weak arrivals there. Lehmann proposed that waves were refracting and reflecting from another boundary deep inside. She never saw the inner core; she inferred it from a disciplined reading of what should not have arrived, but did.







