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Chapter 13 Overview

Authored by Dave Shoff

Biology

9th - 12th Grade

Used 85+ times

Chapter 13 Overview
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31 questions

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1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

The process of change over time is

biodiversity.

geology.

fossilization.

evolution

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Darwin's ideas are relevant today because

they help us understand how organisms change over time.

they give us clues to Earth's biological past.

they help us understand relationships between living things and the natural world

all of the above

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

During his voyage on the HMS Beagle, Darwin noticed that similar habitats in different parts of the world contained

the same plants and animals.

ecologically different plants and animals.

different but ecologically similar plants and animals.

the same fossils.

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Darwin noticed that within a local area, different but closely related species

lived in different habitats.

lived in the same habitat.

competed for food.

competed for mates.

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Darwin drew support for his theory of evolution from the observation that fossils

of some extinct animals are similar to living species.

of dinosaurs prove that dinosaurs once existed on Earth.

belong to ancient species that are now extinct.

share a common ancestor.

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Hutton and Lyell's research suggested that Earth

changes slowly over long periods of time.

has not changed much over time.

now has geological processes that are different than from those in the past.

is only a few thousand years old.

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Darwin's observation of fossils of marine animals found several thousand feet above sea level can be explained by

ancient people moving the fossils to higher ground.

marine animals adapting to live far from the sea.

geological events causing the ancient seafloor to move to a higher elevation.

Darwin's misidentification of fossils.

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