Which statement accurately describes how to reflect point A (3, −1) over the y-axis?

Question 6 options:

Construct a line from A parallel to the x-axis, determine the distance from A to the x-axis along this parallel line, find a new point on the other side of the x-axis that is equidistant from the x-axis.


Construct a line from A perpendicular to the y-axis, determine the distance from A to the y-axis along this perpendicular line, find a new point on the other side of the y-axis that is equidistant from the y-axis.


Construct a line from A perpendicular to the x-axis, determine the distance from A to the x-axis along this perpendicular line, find a new point on the other side of the x-axis that is equidistant from the x-axis.


Construct a line from A parallel to the y-axis, determine the distance from A to the y-axis along this parallel line, find a new point on the other side of the y-axis that is equidistant from the y-axis as A is.

Answers

Answer 1

Answer:

The third option correctly describes how to reflect point A (3, −1) over the y-axis:

Construct a line from A perpendicular to the x-axis, determine the distance from A to the x-axis along this perpendicular line, find a new point on the other side of the x-axis that is equidistant from the x-axis.

Explanation:

Answer 2
The statement that accurately describes how to reflect point A (3, -1) over the y-axis is:

Construct a line from A perpendicular to the y-axis, determine the distance from A to the y-axis along this perpendicular line, find a new point on the other side of the y-axis that is equidistant from the y-axis.

When reflecting a point over the y-axis, you draw a perpendicular line from the point to the y-axis. Then, you determine the distance from the point to the y-axis along this perpendicular line. Finally, you locate a new point on the other side of the y-axis that is equidistant from the y-axis as the original point A.

Related Questions

explain the significance of shadow zones providing the information about Earths interior

Answers

Answer:

Shadow zones help us understand the properties and structure of the planet's layers. When seismic waves, generated by earthquakes or other sources, travel through Earth's interior, they encounter different materials and undergo various changes in their paths and speeds.

P-wave Shadow Zone:

P-waves, also known as primary waves or compressional waves, are the fastest seismic waves and can travel through both solids and liquids. However, they experience refraction and change in speed as they cross boundaries between different layers of Earth's interior. This causes a shadow zone between 103° and 142° from the earthquake's epicenter. In this region, P-waves are not detected on seismographs.

S-wave Shadow Zone:

S-waves, also called secondary waves or shear waves, travel slower than P-waves and can only propagate through solid materials. They cannot pass through Earth's liquid outer core. As a result, a shadow zone is created beyond 103° from the earthquake's epicenter. In this region, S-waves are not recorded on seismographs.

Information the Zones provide ----------------------------------------------------

Outer Core:

The fact that S-waves do not reach the shadow zone beyond 103° indicates that Earth's outer core is liquid. This supports the theory of a molten outer core composed mainly of iron and nickel.

Inner Core:

The presence of P-waves in the shadow zone beyond 103° but not beyond 142° suggests the existence of a solid inner core. P-waves can only pass through the solid inner core, while they are refracted or absorbed in the liquid outer core.

We can map out the shadow zones and use them to infer the properties and boundaries of Earth's internal layers. Which helps us understand the composition, density, and dynamics of the Earth.

Hope this helps!

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