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Search resuls for: "Jules Verne's"


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In 1889, journalist Nellie Bly set off on a trip around the world, trying to make it under 80 days. "You see a huge emphasis being placed on building ships that were ever faster than the previous generation of ships," Goodman said. Once aboard the train, Bly began to receive telegrams from her editors and well-wishers. "Sometimes it literally literally just says, 'Nelly Bly's train,'" Behn said. For Behn, what Bly and Bisland did remains incredible and deserve to be remembered as much as Verne's story.
Persons: Nellie Bly, Elizabeth Bisland, , Jules Verne's, Bly, Bisland, Adrien Behn, Matthew Goodman, Elizabeth Bisland's, Victoria, Augusta Victoria, Henry Guttmann, seasickness, Behn, San Francisco —, Bettmann, Goodman, John Mix Stanley, Said, Getty Images Bly, they'd, Alfred Touchemolin's, voyaged, She'd, James Buchanan, Joseph Pulitzer's, Nelly Bly's, Jules Verne, Thomas Cook, Fogg, Nelly, she'd Organizations: Service, Cosmopolitan, Atlantic, Hulton, Western, Central Pacific, Union Pacific, Union Pacific's Overland, Rockies, Railroad, US, Ships, Suez, Getty Images, Workers, SSPL, Headquarters, Thomas Cook &, Companies Locations: London, New Jersey, New York, California, Blackwell's, of, New York Harbor, Chicago, Omaha, Utah, San, Salt, Union, Iowa, San Francisco, Midwest, Between Nebraska, Sacramento , California, Sierra Nevada, Lake Jessie , North Dakota, Washington ,, Philadelphia, Suez, Europe, Asia, Africa, Britain, India, Port Said, Egypt, Yemen, commonwealths, British, Aden, Colombo, Penang, Hong Kong, Singapore, Ceylon, Yokohama, France, Germany, America, South China, Nevada, Russian Empire, East, North America, London's, Italy, Ireland, United States, Japan, China
The planet's internal structure comprises four layers: a rocky crust on the outside, then a rocky mantle, an outer core made of magma and a solid inner core. This metallic inner core, about 1,500 miles (2,440) wide, was discovered in the 1930s, also based on seismic waves traveling through Earth. Scientists in 2002 proposed that lurking within this inner core was an innermost section separate from the rest, akin to a Russian Matryoshka nesting doll. The researchers were able to differentiate the two regions because the seismic waves acted differently between them. "The latent heat released from solidifying the Earth's inner core drives the convection in the liquid outer core, generating Earth's geomagnetic field," Pham said.
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