Your answer would be inside the nucleus.
There are three particles in an atom. Protons, neutrons, and electrons. Protons and electrons are both charged, with a positive and negative charge, respectively. Neutrons, on the other hand, are not.
Neutrons are found in the nucleus of the atom (along with protons, while electrons float around). Therefore, uncharged particles in an atom would most likely be found inside the nucleus.
Hope this helped!
Ok that is not true at all it serves as a physical border between Mexico and the United States
1)Japan 2)South Korea 3)China 4)North Korea
Not completely sure because we don't really know anything about North Korea but this is my guess :)
Answer:
Temperatures decrease as you move away :D
Explanation:
Temperature range increases with distance from the equator. Also, temperatures decrease as you move away from the equator. This is because the sun's rays are dispersed over a larger area of land as you move away from the equator.
1. In the middle of the continents
The oldest rocks on our planet can be found in the middle of the continental masses. Such places are the interior of Australia, from where the oldest rock have actually been found, Siberia, Central Africa, the interior of Canada, the interior of Brazil... The reason why this is the case is because of the subduction that occurs between the plates. The oceanic plates are the ones that subduct, thus their crust is getting destroyed, so their rocks are younger. The continental plates, on the other hand, are not getting subducted, but instead they either collide with other continental plates, or go above the oceanic plates that subduct below them, thus their crust is usually not destroyed, except on the surface part where the weathering and erosion are taking part.
2. at conservative boundaries
The conservative plate boundaries, more commonly referred to as transform plate boundaries, are the ones where the tectonic plates are sliding past each other. Instead of the plates moving toward each other, or away from each other, at these boundaries the plates are moving in sliding past each other while moving in opposite directions. The pressure between the plates on these boundaries results in cracks in the crust, known as faults, and they are parallel to the plate boundary. Also, these boundaries are very active geologically, and they often cause earthquakes to occur in the surrounding area.