Sea Floor Spreading Google Form

Sea floor spreading answer key.

Sea floor spreading google form.

The lava cools to form new seafloor. Spreading rate is the rate at which an ocean basin widens due to seafloor spreading. The concept of seafloor spreading was put forward by h harry hess an american geologist. Seafloor spreading theory that oceanic crust forms along submarine mountain zones known collectively as the mid ocean ridge system and spreads out laterally away from them.

Due to plate tectonics magma at mid ocean ridges flows through cracks and forms rock when it cools preparation. There are lots of earthquakes that occur in the middle of the atlantic ocean. How does it support sea floor spreading and description. Seafloor spreading is happening at b.

The rate at which new oceanic lithosphere is added to each tectonic plate on either side of a mid ocean ridge is the spreading half rate and is equal to half of the spreading rate. Underwater mountains form from sea floor spreading in the middle of the ocean from hot lava high temperatures earthquakes. Later more lava erupts at the ridge. Further he claimed that continents would be pushed aside by the same forces that cause the ocean to grow.

The new lava pushes the seafloor that is at the ridge. Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor. Molten rock pushes up from the asthenosphere and pushes the plates apart at the mid ocean ridge. Arthur holmes in 1930s discussed the possibility of convection currents.

To understand the concept of seafloor spreading we must first understand some basic concepts that form the cornerstones for the concept of seafloor spreading. The concept of sea floor spreading. This creates new ocean crust. Hot mantle material rises up at mid ocean ridges.

It is an underwater mountain range that forms when magma pushes up on the crust at a divergent boundary. This is a mid ocean ridge. Spreading rates determine if the ridge is fast intermediate or slow. He suggested that new sea floor forms at the oceanic ridges and spread outwards from the line of origin.

The seafloor spreading hypothesis. Convection current theory convection current theory is the soul of seafloor spreading theory. The mid atlantic ridge for instance separates the north american plate from the eurasian plate and the south american plate from the african plate the east pacific rise is a mid ocean ridge that runs through the eastern pacific ocean and separates the pacific plate from the north american. This idea played a pivotal role in the development of the theory of plate tectonics which revolutionized geologic thought during the last quarter of the 20th century.

The seafloor spreading hypothesis brought all of these observations together in the early 1960s.