Formation of Limestone and Carbonate Deposits

Formation of Limestone and Carbonate Deposits

Assessment

Interactive Video

Geology

9th - 10th Grade

Hard

Created by

Nancy Jackson

FREE Resource

10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary way modern limestone forms?

By sedimentation and lithification of calcified organisms

Through volcanic activity

By the accumulation of sand

From the cooling of magma

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What role did stromatolites play in early carbonate formation?

They caused the extinction of early life forms

They were the first to produce calcium carbonate

They increased molecular oxygen, aiding oxidative weathering

They were the first multicellular organisms

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which of the following is a characteristic of Precambrian ooids?

They are smaller than modern ooids

They are larger than Phanerozoic ooids

They are formed by volcanic activity

They are made of silica

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How did carbonate mud primarily form in the Precambrian?

By the accumulation of plant material

By abiotic precipitation from seawater

Through volcanic eruptions

Through the action of large animals

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What event is associated with a decrease in seawater carbonate saturation?

The Great Oxidation Event

The Cambrian Explosion

The extinction of dinosaurs

The formation of the first supercontinent

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the main difference between bio-induced and bio-controlled mineralization?

Bio-induced is indirect and not directly controlled by organisms

Bio-controlled involves no biological influence

Bio-controlled is indirect and not influenced by organisms

Bio-induced involves direct control by organisms

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the significance of the Great Oxidation Event in carbonate formation?

It decreased the availability of calcium ions

It increased the saturation of carbonate ions

It led to the extinction of stromatolites

It caused a decrease in oceanic pH

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