False
Geologists have discovered a lot about the interior composition of the Earth by studying 'S' and 'P' seismic waves. For example, they learned that Earth has a liquid outer core when they noticed that 'S' waves didn't come out on the other side of Earth because they are unable to travel through liquids.
Because the Earth's core is liquid; S-waves can't travel through liquid.
There are two types of waves. There are S waves (sheer waves) and P waves (compressional waves). The S waves won't travel through the outer core because it's a liquid, but the P waves will go through it and continue going through the inner core as well.
You can hear a sound better in a liquid. This is because the molecules in a liquid are much closer together than the molecules in a gas, so vibrations travel much more easily through a liquid.
There is no seismic wave that can only pass through the Earth's mantle. However S-waves can not travel through earth's outer core because it is a liquid.
A geologist does that and he/she studies both the liquid and solid materials of earth.
the mantle
Convection currents are caused by a rising temperature of liquid in the earth's mantle. The risk is that the pressure will build up and, through volcanoes, the liquid will be pushed out. The risk level varies from place to place and is carefully monitored by geologists.
Germany
because the outer core is liquid and the inner core is solid.
The disturbance from an earthquake propagates as a wave. This wave can be either longitudinal or transverse. (Since waves that pass through the Earth's core are always longitudinal, geologists conclude that the Earth is liquid. A liquid won't transport transverse waves.)
because there is a gap throgh it therefore liquid can pass through it (:
when the refrigerant passes through the metering device, some of it starts to flash from a liquid to a gas because
Solid, because it goes through a longer process than the Liquid. Thus, the Liquid doesn't need as much energy as a solid.
Geologists have discovered a lot about the interior composition of the Earth by studying 'S' and 'P' seismic waves. For example, they learned that Earth has a liquid outer core when they noticed that 'S' waves didn't come out on the other side of Earth because they are unable to travel through liquids.
To change a gas to a liquid, you condense it.
S waves cannot travel through the outer core because they can only travel through solids, and the outer core is liquid.