The Law of Superposition and Index Fossils

The Law of Superposition and Index Fossils

Assessment

Interactive Video

Science, Geography, Social Studies

10th - 12th Grade

Hard

Created by

Quizizz Content

Used 1+ times

FREE Resource

The video explains Earth's dynamic geologic history and the methods scientists use to study it. The law of superposition helps determine the relative ages of sedimentary rock layers, with younger layers on top of older ones. Geologists use this law to sequence events in a specific area. To compare distant areas, index fossils are used. These fossils, from organisms that lived during a short time span, help correlate rock layers across distances, indicating they are of similar age.

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5 questions

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1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is one reason scientists have developed methods to study Earth's history?

Geologic changes are too slow to observe directly.

Scientists prefer modern technology over historical records.

Earth's history is well-documented in ancient texts.

There are no written records of Earth's history.

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

According to the law of superposition, where are the younger rocks typically found?

Below older rock layers

On top of older rock layers

In separate locations from older rocks

Mixed with older rock layers

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How do geologists use the law of superposition?

To determine the absolute age of rocks

To find the chemical composition of rocks

To establish the relative age of rock layers

To predict future geological events

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What characteristic makes a fossil an index fossil?

It is from an organism that lived for a long period.

It is the largest fossil in the rock layer.

It is from an organism that lived during a short, specific time.

It is found in multiple rock layers.

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Why are index fossils useful for geologists?

They indicate the presence of valuable minerals.

They help determine the exact age of a rock layer.

They allow correlation of rock layers across different regions.

They show the climate conditions of the past.