Understanding the WGS84 System

Understanding the WGS84 System

Assessment

Interactive Video

Geography

9th - 10th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video explains that Earth is not a perfect sphere but an oblate spheroid, with a difference in equatorial and polar radii. It introduces the WGS84 ellipsoid model, a mathematical reference for measuring Earth's surface. The video discusses how measurements from this model can differ from actual ground levels and highlights the need for local datums in regions like India for precise measurements.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What does the red zone in the Earth's gravity model indicate?

No gravity

Equal gravity

Higher gravity

Lower gravity

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the shape of the Earth called when it is squished at the poles and bulged at the equator?

Cylinder

Oblate spheroid

Perfect sphere

Ellipsoid

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the equatorial radius of the Earth according to the simplified model?

6300 km

6400 km

6378.137 km

6356.752 km

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the WGS84 ellipsoid primarily used for?

Measuring gravity

Measuring time

Measuring temperature

Measuring position and height

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Where is the coordinate origin of the WGS84 ellipsoid located?

At the South Pole

At the equator

At the Earth's center of mass

At the North Pole

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Why might the WGS84 system not be perfect for very accurate measurements everywhere?

It is too complex

It does not account for local area distortions

It is outdated

It is too expensive

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What might happen if you are at sea level in relation to the WGS84 ellipsoid?

The ellipsoid might be below you

The ellipsoid might be above you

The ellipsoid might be at the same level

The ellipsoid might disappear

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