Alfred Wegener
Alfred Wegener
Research about the seafloor in the second half of the 1900s, particularly the discovery of mid-ocean ridges and magnetic striping patterns, provided strong evidence supporting the theory of plate tectonics. This new understanding of the seafloor helped scientists realize that the seafloor was spreading at mid-ocean ridges, leading to the acceptance of continental drift as part of the larger theory of plate tectonics.
i need to now what the navy made to communicate in the early 1900's
they used the magnifier to launch the band to map the mid-ocean ridge
Yes, in the early 1900s, Russian biochemist Alexander Oparin proposed the hypothesis that life on Earth originated from simple organic compounds through a series of chemical reactions in a "primordial soup." His ideas, presented in his 1924 work "The Origin of Life," suggested that conditions on early Earth could facilitate the formation of complex molecules leading to life. Oparin's hypothesis laid the groundwork for subsequent research in abiogenesis, although it has evolved with new scientific discoveries over the years.
They succeeded in passing four constitutional amendments that changed society.
George Washington carver
Albert Einstein became a scientist in the late 19th century, during his early adult years after completing his formal education. He started publishing scientific papers in the early 1900s, which eventually led to his groundbreaking work on the theory of relativity.
Darwin did not know the mechanism for heredity, and in particular, could not explain how a favorable mutation could become widespread in a species.Mendel's work later explained this to the scientist in the 1900s
no i think the 2oth century is the 1900s?
1900s
Research on the sea floor, such as magnetic striping and age dating of rocks, provided strong evidence for plate tectonics and continental drift in the second half of the 1900s. These findings helped to change scientific thought, as they demonstrated the movement of lithospheric plates and provided a mechanism for how continents move and interact on Earth's surface. This research revolutionized our understanding of Earth's geology and led to the acceptance of the theory of plate tectonics in the scientific community.