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What is the difference between between the lower and upper mantle?
The upper mantle is harder than the lower mantle
What is the difference between the mantle and a convergent plate boundary?
The mantle is below the plates.
What is the relationship between arthropod appendage?
a rope
What is another word for handful?
Multi-fingered grasping appendage. The difference between hands, paws, claws and talons is opposable thumbs.
What is the relationship between arthropod-appendage?
They start with letter a
The distinction between the crust and mantle is primarily on the basis of a difference in?
composition — the crust is primarily composed of lighter, silicate minerals like granite and basalt, while the mantle is composed of denser minerals like peridotite. This compositional difference contributes to variations in density, temperature, and behaviour between the crust and mantle layers of the Earth.
What is the dangly appendage in the back of your throat that is located between your tonsils?
The uvula
What is the difference between Mohorovicic discontinuity and Gutenberg discontinuity?
The Mohorovicic discontinuity, or Moho, is the boundary between the Earth's crust and mantle, marking a change in seismic wave velocity. The Gutenberg discontinuity is the boundary between the Earth's mantle and outer core, where seismic waves change velocity and nature. Essentially, the Moho separates the crust and mantle, while the Gutenberg discontinuity separates the mantle and outer core.
What is the name of the appendage of a fish?
Which appendage.
What divides the mantle and the core?
The boundary separating the Earth's mantle and core is known as the core-mantle boundary. This boundary is characterized by a sharp decrease in seismic wave velocities, indicating a difference in composition and properties between the outer core and the lower mantle.
What part of speech is appendage?
Appendage is a noun.
What is the difference between the Mohorovicic discontinuity and the Gutenberg discontinuity?
The Mohorovicic discontinuity (Moho) is the boundary between the Earth's crust and mantle, where seismic waves change velocity. The Gutenberg discontinuity is the boundary between the Earth's mantle and outer core, characterized by a sharp increase in seismic wave velocities.
