<span>B. Aggregate. Stone, gravel, and other bits of crushed rock are known as the 'aggregate' in Earth Science, as they are made up of the aggregation of extraneous bits of stone. They are a nonrenewable resource which we rarely think about, but which is utilized for a number of different industries and day-to-activities. It can be man made as well as naturally occurring.</span>
Answer:
Explanation:
GIS stands for Geographic Information Systems.
GIS is an environment which is used for collecting, storing, manipulating, analyzing and visualizing geographical data.
The most important aspect of GIS is its capability in handling data with locational attributes which are geographical data.
To use data from the database from a chain of hardware stores, the data must be tied to their respective location i.e they must locational attributes.
Question:
If you lived on Mars and observed the solar system from there, _____________ would describe retrograde loops, ______________ would always be seen near the sun, and _________________ would never be visible as crescent phases
Answer:
1. All other planets
2. Mercury, Venus, and Earth
3. Jupiter and Saturn
Explanation:
Living on Mars, all other planets would describe the retrograde loops, while the inner planets (Mercury, Venus, and Earth
) would always be seen near the sun. Planets like the Jupiter and Saturn which are far away from the sun will never have a crescent phase as those that will have a crescent phase must be between the mars and the sun
The name of the island is honshu
When a mid-ocean ridge is offset, the linear feature connecting and between the crests of the ridge segments is called a Transform Fault.
As the Earth's tectonic plates separate, new ocean bottom is generated along divergent plate borders, which are known as mid-ocean ridges. Massive basalt volcanic eruptions result from molten rock rising to the seafloor as the plates divide. A ridge's shape is influenced by how quickly it spreads; slower spreading rates produce steep, erratic topography, while faster spreading rates result in much wider profiles and kinder slopes.
In geology and oceanography, a transform fault is a type of fault when two tectonic plates slide past one another. A transform fault may develop in the area of a fracture zone that connects spreading centres to deep-sea trenches in subduction zones or that lies between various offset spreading centres.
In the 1960s, Morgan postulated that spreading centres and transform faults separate opposing plates along an oceanic ridge crest that is offset by fracture zones.
The direction of motion on the transform faults was predicted by Morgan's hypothesis to be opposite to the offsets of the ridge crests, which was a rather dramatic assertion.
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