Abyssal plains are large, flat features that cover about one third of the planet.
<h3>What are Abyssal plains?</h3>
- The broad, flat, sediment-covered regions of the deep ocean floor are known as abyssal plains.
- They have a slope of less than one foot of height variation for every thousand feet of travel, making them the flattest, featureless places on Earth.
- When tectonic plates separate, magma rises and forms new crust, filling the space that was left between the plates.
- When sediments from the shoreline pass over the continental shelf, tumble down the continental slope, and deposit on top of the more recent oceanic crust, they create an abyssal plane.
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Answer:
They are used to find the distance between two hills.
Explanation:
Scale bars in a topographic map is used to find the distance between two hills.
The bar shows the relationship between ground distance and that map distance.
- When we compare the distance measured on map with the scale given, we can find the true distance on land.
- Scales are mostly used for abstracting the real world.
Answer:
Vertical dimension
Explanation:
The third dimension used by geologists and map users is the vertical dimension.
It brings a volumetric angle to geological problems.
- For geologists, rock strata can be viewed downhole.
- It does not limit dimensional analysis to the area of the body, it brings a volumetric approach.
- Sometimes, in geologic literature, it is termed a slice through the rock.
- The third dimension makes the map figure real and more interactable.
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Answer:
Explanation:
Globalization has brought benefits in developed countries as well as negative effects. The positive effects include a number of factors which are education, trade, technology, competition, investments and capital flows, employment, culture and organization structure.
