Discontinuity
Rock
Rock
To change density there are three ways. You can change the shape, mass or volume of the object
When mass increases and volume stays constant, the density increases. When volume increases and mass stays constant the density decreases. When they both change, then the density will depend on the rate of change of mass and the rate of change of volume.
Density does not change regardless of where the object is. It is a constant.
Density usually changes when an object is heated or cooled - especially in the case of gases, or when there is a change of phase.
It is unchanged. The density is the mass divided by the volume, and as both of these numbers are halved the density does not change.
Abrupt means quick or fast, so the phrase abrupt change means an altered course that is made fast or quickly.
The motorcyclist made an abrupt lane change.
The government made an abrupt change in their policy.
Yes, as changes in salinty affects the density of sea water, another of putting it would be that a Halocline is simply a region below the surface of a body of water where there is a significant increase or decrease in density.
yes
feedback loops
A waterfall occurs when naturally flowing water undergoes an abrupt change in distance above sea level.
mantle plumes
Arrange the letters of the word "abrupt" vertically, then write a word or phrase starting with each letter that relates to the theme of "abrupt." For example, "Abrupt change," "Bold and unexpected," "Rapid shifts," "Unexpected interruption," "Pointed actions taken."
The Gutenberg Discontinuity is the mantle/core boundary within Earth's interior where there is an abrupt change in the seismic waves (generated by earthquakes or explosions) that travel through Earth. It is at a depth of about 1,800 mi (2,900 km) below the surface.
''There was an abrupt change in the child's behaviour''The term ''abrupt'' is used as:Sudden and unexpectedIt is also use to show ''Rudeness''It is pronounced as: ab·rupt/əˈbrəpt/Hope that was helpfulBy: Anabela L.
The Gutenberg Discontinuity is the mantle/core boundary within Earth's interior where there is an abrupt change in the seismic waves (generated by earthquakes or explosions) that travel through Earth. It is at a depth of about 1,800 mi (2,900 km) below the surface.