read ur notes or the paragraphs daa
Strength Activator Plate Movement The movement of tectonic plates can occur because of the relative density of oceanic lithosphere and asthenosphere is relatively weak character. The release of heat from the mantle has been found, the original source of energy that drives plate tectonics. Approved view now, though still quite debatable, is that the excess density of oceanic lithosphere that makes infiltrate downward in subduction zones is the most powerful source of plate movement. At the time of its formation in mid-ocean ridge, oceanic lithosphere initially have a lower density than the surrounding asthenosphere, but this density increases with aging due to cooling and thickening. The magnitude of the density of old lithosphere relative to the underlying asthenosphere allows the infiltration into the mantle at subduction zones so that the source of most of the driving forces-the movement of plates. Weakness of the asthenosphere allows the plates to move easily towards a subduction zone [19] Although subduction is believed to be the strongest force driving plate-movement, there is another driving force plate as evidenced by the North American plate, Eurasian plate is also moving but did not experience subduction anywhere. Driving source is still a topic of intensive research and discussion among scientists of earth sciences. Two and three-dimensional imaging of the Earth's interior (seismic tomography) shows a heterogeneous density distribution throughout the mantle laterally.Variations in density may be material (from rock chemistry), mineral (from variations in mineral structure), or thermal (through thermal expansion and contraction from heat energy). Manifestation of the lateral density heterogeneity is mantle convection from buoyancy forces (buoyancy forces) [20] How mantle convection relates directly and not by movement of the planet is still a field that is being studied and dealt in geodinamika. With one way or another, this energy must be transferred to the lithosphere that the tectonic plates to move. There are two main types of styles that influence the movement of planets, ie friction and gravity.
Yes, Earth is layered primarily due to differences in density among its materials. Heavier elements, like iron and nickel, sank to form the core, while lighter materials formed the mantle and crust. This stratification occurred during the planet's formation, as heat caused materials to melt and differentiate based on their densities. The resulting layers—crust, mantle, outer core, and inner core—reflect these variations in composition and density.
yes
Saturn has the lowest density, but it has more than 31 moons.
Studying embryos of animals with backbones can help elucidate evolutionary relationships by identifying similarities and differences in developmental processes. By comparing developmental stages and gene expression patterns, researchers can infer common ancestry and evolutionary relationships among different species. This information can provide insights into the evolutionary history of vertebrates and help reconstruct their phylogenetic relationships.
At the bottom of a graphic organizer that show relationship among heat, movement, and density in mantle rock. Also when it sinks the mantle rock starts to be heated up once again.
At the bottom of a graphic organizer that show relationship among heat, movement, and density in mantle rock. Also when it sinks the mantle rock starts to be heated up once again.
The mantle rock would be densest where it is closest to the Earth's core, which is at the boundary between the mantle and the outer core. This is due to the high pressure and temperature conditions at this depth.
The core has the highest density among the crust, mantle, and core. This is because the core is composed mainly of iron and nickel, which are heavy elements that increase its overall density compared to the other layers of the Earth.
The mantle is typically divided into the upper mantle (including the lithosphere and asthenosphere) and the lower mantle. The upper mantle is rigid and brittle, while the lower mantle is more plastic and capable of flow. The upper mantle plays a crucial role in plate tectonics, whereas the lower mantle's convection currents are thought to drive the movement of tectonic plates.
Essentially, then, the scientific management movement emphasized a concern for output, while the behavioral science movement stressed a concern for relationships among workers.
Radon gas has the highest density among all gases.
Strength Activator Plate Movement The movement of tectonic plates can occur because of the relative density of oceanic lithosphere and asthenosphere is relatively weak character. The release of heat from the mantle has been found, the original source of energy that drives plate tectonics. Approved view now, though still quite debatable, is that the excess density of oceanic lithosphere that makes infiltrate downward in subduction zones is the most powerful source of plate movement. At the time of its formation in mid-ocean ridge, oceanic lithosphere initially have a lower density than the surrounding asthenosphere, but this density increases with aging due to cooling and thickening. The magnitude of the density of old lithosphere relative to the underlying asthenosphere allows the infiltration into the mantle at subduction zones so that the source of most of the driving forces-the movement of plates. Weakness of the asthenosphere allows the plates to move easily towards a subduction zone [19] Although subduction is believed to be the strongest force driving plate-movement, there is another driving force plate as evidenced by the North American plate, Eurasian plate is also moving but did not experience subduction anywhere. Driving source is still a topic of intensive research and discussion among scientists of earth sciences. Two and three-dimensional imaging of the Earth's interior (seismic tomography) shows a heterogeneous density distribution throughout the mantle laterally.Variations in density may be material (from rock chemistry), mineral (from variations in mineral structure), or thermal (through thermal expansion and contraction from heat energy). Manifestation of the lateral density heterogeneity is mantle convection from buoyancy forces (buoyancy forces) [20] How mantle convection relates directly and not by movement of the planet is still a field that is being studied and dealt in geodinamika. With one way or another, this energy must be transferred to the lithosphere that the tectonic plates to move. There are two main types of styles that influence the movement of planets, ie friction and gravity.
By definition, density = mass / volume.
sociology
it is studied as ecology. relationships are responses, mineralisation, locomotion etc to the environment
Ecumenical movement