The intensitylevels I of two earthquakes measured ona seismograph can be compared by the formula log I 1 I 2 = M 1 − M 2 where M is the magnitude given by the Richter Scale. In August 2009 , an earthquake of magnitude 6.1 hitHonshu, Japan. In March 2011 , that same regionexperienced yet another, more devastating earthquake, this time with a magnitude of 9.0. [ 23 ] Haw many timesgreater was the intensity of the 2011 earthquake?Round to the nearest whole number.
The intensitylevels I of two earthquakes measured ona seismograph can be compared by the formula log I 1 I 2 = M 1 − M 2 where M is the magnitude given by the Richter Scale. In August 2009 , an earthquake of magnitude 6.1 hitHonshu, Japan. In March 2011 , that same regionexperienced yet another, more devastating earthquake, this time with a magnitude of 9.0. [ 23 ] Haw many timesgreater was the intensity of the 2011 earthquake?Round to the nearest whole number.
The intensitylevels I of two earthquakes measured ona seismograph can be compared by the formula
log
I
1
I
2
=
M
1
−
M
2
where M is the magnitude given by the Richter Scale. In August
2009
,
an earthquake of magnitude
6.1
hitHonshu, Japan. In March
2011
,
that same regionexperienced yet another, more devastating earthquake, this time with a magnitude of
9.0.
[
23
]
Haw many timesgreater was the intensity of the
2011
earthquake?Round to the nearest whole number.
Consider the table of values below.
x
y
2
64
3
48
4
36
5
27
Fill in the right side of the equation y= with an expression that makes each ordered pari (x,y) in the table a solution to the equation.
solving for x
Consider the table of values below.
x
y
2
63
3
70
4
77
5
84
Fill in the right side of the equation y= with an expression that makes each ordered pari (x,y) in the table a solution to the equation.
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How to determine the difference between an algebraic and transcendental expression; Author: Study Force;https://www.youtube.com/watch?v=xRht10w7ZOE;License: Standard YouTube License, CC-BY