Answer:
Step-by-step explanation:
Ice sheets have one particularly special property. They allow us to go back in time and to sample accumulation, air temperature and air chemistry from another time[1]. Ice core records allow us to generate continuous reconstructions of past climate, going back at least 800,000 years[2].
Ice coring has been around since the 1950s. Ice cores have been drilled in ice sheets worldwide, but notably in Greenland[3] and Antarctica[4, 5]. High rates of snow accumulation provide excellent time resolution, and bubbles in the ice core preserve actual samples of the world’s ancient atmosphere[6].
Answer:
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Step-by-step explanation:
From Analytical Geometry we get that linear functions can be found after knowing a point and its slope. The standard form of a linear function is represented by the following formula:
(Eq. 1)
Where:
- Independent variable, dimensionless.
- Dependent variable, dimensionless.
- Slope, dimensionless.
- y-Intercept, dimensionless.
At first we need to calculate the y-Intercept, which is cleared within (Eq. 1):
If we know that 
, 
and 
, then the y-Intercept of the linear function is:
Line with a slope of 
that goes through the point (2, 1) is represented by 
.
Lastly, we graph the line by using a plotting software (i.e. Desmos), whose result is included below as attachment.
If the matrix is a nonsingual then two strategies must be properties
More pipes less time.
5 pipes means 1h ergo 10 pipes means half, that is 30min.
Hope this helps.
Angle g= 180-60-67=120-67=53
so they are similar three angle is the same
