In 1936, Danish seismologist Inge Lehmann analyzed travel-time graphs of faint seismic compressional waves (-waves) recorded at stations situated within the deep 'shadow zone'—an angular distance between approximately and from an earthquake's epicenter where direct -waves were theoretically absent due to refraction at the mantle-core boundary. Prior models, established primarily by Beno Gutenberg, treated the Earth's core as a single homogeneous liquid shell that bent -waves downward, creating this shadow zone. Gutenberg and his contemporaries attributed anomalous -wave arrivals detected within the shadow zone exclusively to lateral diffraction around the core's outer perimeter or to instrumental noise. Lehmann demonstrated that diffraction could not account for the observed sharpness and high frequencies of these shadow-zone phases. Instead, she hypothesized a concentric, higher-velocity inner core possessing a distinct physical boundary that refracted and reflected -waves into the shadow zone. Although Lehmann refrained from definitively asserting the physical state of matter of this inner sphere, her calculations showed that a sudden velocity increase across a sharp discontinuity within the core matched empirical arrival times.
Which of the following statements can be properly inferred from the passage? (Select all that apply)
- Under Gutenberg's model, direct compressional waves were presumed to follow paths that bypassed surface monitoring stations situated between and from an epicenter.Answer
- Diffracted seismic waves typically exhibit lower frequencies or less distinct arrival profiles than the shadow-zone phases Lehmann evaluated.Answer
- CLehmann conclusively demonstrated that the newly hypothesized inner core had to be in a solid state because liquids cannot transmit compressional waves.
- DSeismic monitoring stations located outside the to angular range were incapable of recording reflected seismic phases from the inner core boundary.
- EGutenberg's contemporaries modified seismograph sensitivity parameters to suppress spurious readings caused by ambient mechanical vibrations.