Answer:
You need to satisfy the equation.
I will solve one.
Step-by-step explanation:
x -2 < -5
now add + 2 to both sides to keep its value.
now we end up with x <-3, which means that the value of x should be less than -3 in order to satisfy the equation.
So -5 is an answer, -4 is an answer, but not -3 because it should be less than -3 not equal.
As for number 9 the dash underneath the less than symbol means that it can equal to.
Hope this helps.
Answer: The answer is (1)
Step-by-step explanation: ( 1 + 1 ) = 2
2 ÷ 2 = 1
~Hope this helps, have a great day/night!~
The coefficient does not determine whether a function is a polynomial or not but the degree of the polynomial.
Multiplying polynomial expressions
Given the following product of the polynomial as shown below
10x^4 * 0.5x^3
Multiply the decimal and the exponent to have;
10x^4 * 0.5x^3
(10*0.5) *(x^4 * x^3)
(10*1/2) * (x^4+3)
(5)x^7
Hence the product of the given polynomial function is 5x^7
The error in Han's thinking is by assuming 0.5x^3 is not a polynomial because 0.5 is not an integer. The coefficient does not determine whether a function is a polynomial or not but the degree of the polynomial.
Learn more on polynomial here: brainly.com/question/24380382
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I believe A, C, D, E, and G. I don't know if I am right, I am just making an educated guess. Please tell me if I am right!
The complete question is:
Which statements describe the location of an earthquakes epicenter? Check all that apply.
1) it is measured by a seismograph
2) is is located using a single set of data
3) it is determined by the arrival times of s and p waves
4) it is determined by the arrival time of surface waves
5) it is located at the point where circles intersect on a map
Answer:
The answers are; 1, 3 and 5.
Step-by-step explanation:
A Seismograph is a combination of centimeters with a timing device and a recording device. It is used to locate and characterize earthquakes, and to study the Earth's internal structure.
Seismograph are not enough to locate the epicenter through Triangulization. The epicenter can also be extrapolated by using an extrapolation map that deduces the distance to epicenter using the difference in time between the arrival of the s and p waves of the earthquake.
