Answer: coordinates such as latitude and longitude
Explanation: A place's absolute location is its exact place on Earth, often given in terms of latitude and longitude. For example, the Empire State Building is located at 40.7 degrees north (latitude), 74 degrees west (longitude). It sits at the intersection of 33rd Street and Fifth Avenue in New York City, New York.
Changes in the supply source or sediment supply can begin or end the life of a river.
<h3>What other factors can affect the life of a river?</h3>
Other factors that can affect the life of a river are;
- The kind of rocks present on the shores
- The source and supply of sediments.
Sediments deposited continually on the shores of a river can gradually edge the river away from it's course or cut it off from it's source.
Hence, it is right to state that Changes in the supply source or sediment supply can begin or end the life of a river.
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less far fetched
Explanation:
When plate tectonics was discovered, Wegener's continental drift theory became less far fetched.
Alfred Wegener in 1912 proposed the theory of continental drift. He provided a wide array of evidence to support his claims.
- His idea was not accepted by the scientific community of his days.
- There was no mechanism available and known to account for the moving plates.
- Late on through the years, the idea of mantle convection came into lime light around 1930.
- By 1960, the theory sea floor spreading was already established.
- This lead to the advent of the theory of plate tectonics.
- In the end, the theory of Continental drift became less far fetched and better understood.
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I think there is a mistake in the subject area. This has nothing to do with geography, but with physics. This topic is about the linear expansion of conductive materials when heated to a higher temperature. The equation for linear expansion is
ΔL = L0*α*ΔT, where
ΔL is the change in length when heated
L0 is the original length of the rod
α is the coefficient of linear expansion; this is an empirical data for a specific kind of material
ΔT is the change in temperature
Since ΔL is same for lead and quartz, we can equate them.
L0,lead*α,lead*ΔT = L0,quartz*α,quartz*ΔT
The α for lead is 29×10^6 °C/m while the α for quartz is 14×10^6 °C/m. Since ΔT are the same for both materials, ΔT will be cancelled out. Therefore, the equation for L0,quartz is:
L0,quartz = (L0,lead*α,lead)/α,quartz
L0,quartz = (0.10 m*29×10^6 °C/m)/14×10^6 °C/m
L0,quartz = 0.207 m
Answer:
answer d-created by differences in temperature and saltiness
Explanation: