In 1905, geologist Richard Dixon Oldham analyzed seismic waves generated by the 1897 Assam earthquake to investigate Earth's internal structure. By comparing the arrival times of primary (P) and secondary (S) waves at recording stations globally, Oldham identified a distinct shadow zone beyond 104 degrees from the epicenter where direct S-waves failed to emerge. From this specific absence, Oldham deduced the existence of a central fluid core that impeded shear wave transmission. However, because his instruments lacked the sensitivity to detect faint, refracted P-waves passing through the deepest interior, Oldham incorrectly estimated the core's radius to be substantially larger than modern measurements indicate, attributing the wave attenuation entirely to homogenous core density rather than a distinct solid inner core boundary.
Based on the passage, which of the following statements regarding Richard Dixon Oldham's 1905 seismic investigation are explicitly supported? Consider each of the three choices separately and select all that apply.
- Oldham's deduction of a fluid central core relied on observing the absence of direct S-waves at stations located more than 104 degrees from the earthquake's epicenter.Answer
- BOldham correctly calculated the precise radius of the Earth's core by measuring the speed of refracted P-waves.
- The seismological recording instruments available to Oldham failed to register faint P-waves passing through the planet's deepest interior.Answer