SECTION 2.3
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Equations of Lines: Making Linear Models 165
(a) Use the graph to decide which of them is traveling faster.
(b) Find the speed at which each of them is driving.
(c) Find linear functions that model the distances that Jade and Jari travel as functions
of t.
60. Sedimentation Rate Geologists date geologic events by examining sedimentary
layers in the ocean floors. For instance, they can tell when an ancient volcano erupted
by noting where in the sedimentary layers its ash was deposited. This is possible
because the rate of sedimentation is assumed to be largely constant over geologic eras,
so the depth of the sedimentation is modeled by a linear function of time. To examine
sedimentary strata, core samples (often many meters long) are drilled from the ocean
floor, then brought to the laboratory for study. Special features in the layers, including
the chemical composition of the deposits, can indicate climate change or other geologic
events. It is estimated that the rate of sedimentation in Devil’s Lake, South Dakota, is
0.24 cm per year. The depth beneath the lake bottom at which a layer of sediment lies is
a function of the time elapsed since it was deposited.
(a) Find a linear function that models the depth of sediment as a function of time
elapsed.
(b) To what depth must we drill to reach sediment that was deposited 300 years ago?
20
10
30
2468
Jade
Jari
Time since 7:00
A.M.
min
Distance
traveled (mi)
10 12
(6, 7)
(6, 16)
0
t
y
Examining core samples
© Charles O. Cecil/Alamy
2
2.3 Equations of Lines: Making Linear Models
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Slope-Intercept Form
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Point-Slope Form
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Horizontal and Vertical Lines
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When Is the Graph of an Equation a Line?
IN THIS SECTION… we find different ways of representing the equation of a line. These
help us to construct linear models of real-life situations in which we know “any two points”
or “a point and the rate of change”of a linear process.
GET READY… by reviewing Section 1.3, particularly how linear models are constructed
using the “rate of change” and “initial value” of a linear process.
In Section 2.2 we learned that the graph of a function with constant rate of change is
a line. We also saw that linear functions are useful in modeling many real-world sit-
uations. To find a linear model, we needed to know the “initial value” and the “rate
of change” (or “y-intercept” and “slope”). But often this particular information is not
available: We might know the rate of change and a particular value but not the initial
value, or we might simply know two values of the linear function.