Answer:
Explanation:
A region is an area of land that has common features. A region can be defined by natural or artificial features. Language, government, or religion can define a region, as can forests, wildlife, or climate. Regions, large or small, are the basic units of geography.S
The oceanic lithosphere consists of the upper part of the Earth's crust that is submerged beneath the oceans. It is primarily made up of basalt, but can consist of other forms of sediment deposited by rivers or currents; the basalt feature exists due to the oceanic lithosphere's creation via divergent tectonic activity. The continental shelf is a portion of the crust that is of higher elevation than the rest of the ocean due to its connection to the less dense continental lithosphere. The continental slope, therefore, is the portion of the crust where the continental shelf decreases in elevation as it meets the denser oceanic lithosphere. Abyssal plains are portions of the lithosphere far from spreading centers - they consist of rocks older than those near rifting centers. Due to the coolness of the plate and their distance from rifting centers, abyssal plains are some of the lowest continuous portions of the lithosphere (cool rock is denser and thus sinks to a lower elevation). Since they are very much inactive, abyssal plains are coated with sediment and are very, very flat.
Answer:
Different parts of Earth's surface receive different amounts of sunlight. The sun's rays strike Earth's surface most directly at the equator. ... Because of the Earth's tilt the sun's rays strike the surface at a slant at the poles; they are less focused. This spreads the rays over a wide area.
A typical passage through the panama canal would take 8-10 hours
The correct answer is - True.
The transform boundaries of the tectonic plates are boundaries where two tectonic plates are sliding against each other. As they do that, they do create geological activity around the boundary, and earthquakes are a common occurrence. Another trademark of these boundaries are the faults, that stretch for several km in a linear manner, usually parallel to the boundary itself. Most of these faults are located in the ocean basins and they are connecting the offsets of the mid-ocean ridges, but they can also be found on land, like it is the case in California.
