Answer:
A one-step conversion is not sufficient to convert a temperature in the Celcius scale to the Fahrenheit scale.
Explanation:
Hello!
To convert a temperature in the Celcius scale to the Kelvin scale we required just one-step conversion, because we consider that the first scale derives from the second scale.
Celcius scale begins at 0 degrees (0°C), wich coincides with the melting point of the ice, and ends at 100 degrees (100 °C) with the point of water boiling point.
Fahrenheit scale determines that the freezing point of water is located at 32 degrees (32°F) and its boiling point at 212 degrees (212°F). This situation causes a 180 degree interval between the two points.
For this reason, to calculate how many Fahrenheit degrees has a certain temperature expressed in Celcius degrees, we have to multiply the X degrees Celcius (°C) by 1.8, and then add 32 to the previously obtained result.
°F= (X°C x 1.8) + 32
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1. There are three types of tectonic plate boundaries and they includes:
- When two plates slide past each other, they form a <u>transform boundary</u>.
- The <u>divergent boundary</u> occurs when two plates pull away from each other.
- When two plates collide with each other, they formed a <u>convergent boundary</u>.
2. The newest parts of the Earth’s crust is located at mid-ocean ridges.
- The mid-ocean ridge refers to the seafloor mountain system formed by plate tectonics and are the newest parts of the Earth’s crust.
3. Not every earthquake has a foreshock, but every earthquake has aftershock that occur in places far away from the mainshock.
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<em>brainly.com/question/16177163</em>
Answer:
I think its ans is option B
The answer is B. In a destructive plate boundary, the descending plate, usually the oceanic plate begins to melt as it descends below into the mantle. This forms magma that rises and erupts onto the overlying continental plate through fissures. This volcanic activity is responsible for geographical features such as the volcanic island arc, which lies parallel to the subduction zone.
Answer:
The Precambrian history of Earth is difficult to determine for all of the following reasons except e. There are few useful index fossils in the Precambrian record .
Explanation:
Precambrian history
Precambrian history is difficult to study as there are relatively low Precambrian fossils and most of the Precambrian rocks have metamorphosed and ,
there are few useful index fossils in Precambrian record as it is well known the evolution of life on earth was not very predominant in Precambrian time.
