its A
Explanation:
atmosphere at a place and a time as regards heat, dryness and sun sunshine also winds n rain and more.
Answer:
The factor that plays a signficant role in the shifting of both voting patterns and district boundaries is population.
Explanation:
In the United States, district boundaries and voting patterns are largely dependent on population. This is one reason why the national census carried out in the United States every 10 years is so important. The information from the Census is used to delegate federal money for government programs, it is used by the Department of Education for school district information, and it is also the basis for drawing up congressional district boundaries and for assessing voting patterns. In most states, the district boundaries are decided by the state legislature and both chambers have to approve the boundary plans in the majority. In some states, the governor has the power to veto this decision, but in others, he does not. In recent years there have been criticisms of this system because it can be subject to political manipulation where through gerrymandering a party tries to divide up a district, for example. This happens when say a poor neighborhood that wants to vote Democrat is split between two neighborhoods that vote Republican so that the Republican wins both seats more easily.
Answer:
the map matches C.
Explanation:
the map shows an elevated land with a flat top, also known as a plateau. image C shows a plateau, therefore the map matches C.
hope this helps
Answer:
Explanation:
The three main types of volcanoes are as follows:
1. Composite volcanoes: These are also called as strato volcanoes. These are steep and formed by the layers of ashes and lava. The eruption from these volcanoes is in the form of pyroclastic flow. The pyroclastic flow is in the form of superheated mixture which consists of rock dust, ash, and hot steam. These volcanoes can rise above the 8000 feet. These are found in the destructive plate margins. Example of these volcanoes include the Mount Fuji in Japan.
2. Shield Volcanoes: These volcanoes are low and they have gentle sloping sides. These are formed by the layers of lava. Their eruption of lava is non-explosive. These produces the fast flowing fluids that can flow to many miles. These can destroy the nearby surrounding regions can cause injury and even death. These volcanoes are found in the region of constructive boundaries and also at the volcanic hotspots. The examples of shield volcanoes include the Maunaloa on Hawaii.
3. Dome volcanoes: These are also called as acid lava cones as these emit acid which is much thicker than that of the lava. These have steeper sides as compared to the shield volcanoes. The lava is thick and sticky as a result of this it cannot flow to far region and it cools and solidifies. The example of dome volcanoes include the Puy de Dome of Auvergne, France.
