Continental drift Continental drift Continental drift is the theory that the Earth's continents have moved over geologic time relative to each other, thus appearing to have "drifted" across the ocean bed. The speculation that continents might have 'drifted' was first put forward by Abraham Ortelius in 1596. The concept was independently and more fully developed by Alfred Wegener in 1912, but his theory was rejected by many for lack of any motive mechanism. Arthur Holmes later proposed mantle convection for that mechanism. The idea of continental drift has since been subsumed by the theory of plate tectonics, which explains that the continents
A Discourse on the Study of the Law of study at a University. He was particularly alarmed by the growing practice of sending a potential lawyer to work in an attorney's office, saying that: In Continental Europe and Scotland, the academic study of the law was regarded as a required part of a gentleman's training, but it was not in England; the aristocracy "have been more remarkably deficient than those of all Europe". This was because the "stylistic barbarisms and crafty practitioners" were seen as below the aristocracy, and not conforming to gentleman-like sensibilities. Blackstone also emphasised the need for gentlemen to study not only the law, but