Answer:
Fast changes occur through the actions of Earthquakes, volcanoes, landslides, etc. over short periods of time
hopefully this helps
This is due to the amount of infrastructure in the city. All that metal holds heat making inside the city hotter than outside the city.
Answer:
Hello. You have not attached the map to which this question refers, which makes it impossible for your question to be answered. However, I can help you by showing that the political map can be used by a historian who wants to study the distribution and division of Roman society within Roman territory.
Explanation:
A political map is used when a stylist wants to analyze the administrative division of a territory, showing the border of that territory with neighboring territories and also showing the internal borders that show the divisions within the territory.
In this case, we can say that a historian would use a political map to analyze the geographic distribution and population concentrations of Roman civilization.
Surface, crust, mantle, and core
Slowly, deep underground
The igneous rock gabbro is coarse grained and non-vesicular. Both characteristics show that it is an intrusive igneous rock. Intrusive igneous rocks are formed below Earth's surface and slowly (because they're underground). When rocks are intrusive, they are are non-vesicular (no air pockets) because the air has had the time to escape because of the slow cooling time period. Intrusive rocks are also coarse because crystals had the time to form in the rock during that longer cooling time.
Ps. extrusive igneous rocks form rapidly at Earth's surface and basically have tge opposite characteristics for the opposite reasons (ex: vesicular cause air had little time to escape)
