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Covalent Structures and Properties

Covalent Structures and Properties

Assessment

Interactive Video

Chemistry, Science, Physics

9th - 10th Grade

Practice Problem

Hard

Created by

Patricia Brown

FREE Resource

The video tutorial explains network covalent bonding, contrasting it with molecular structures. It highlights the properties of substances like methanol, carbon dioxide, and hydrogen cyanide, which have lower melting points due to weak intermolecular forces. In contrast, network covalent structures like diamond and quartz are strong and have high melting temperatures due to extensive covalent bonding. Diamond's structure is detailed, showing each carbon atom bonded to four others, forming a robust network. Quartz, a common mineral in the earth's crust, also exemplifies network covalent bonding, contributing to its strength and high melting point.

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5 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is a key difference between molecular structures like methanol and network covalent structures?

Molecular structures have higher melting points.

Network covalent structures are made of individual atoms not bonded together.

Network covalent structures have weaker forces between atoms.

Molecular structures consist of discrete molecules with space in between.

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

In a diamond structure, how many other atoms is each carbon atom bonded to?

Three

Five

Two

Four

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Why does diamond have a high melting temperature?

Due to the presence of hydrogen bonds.

Because of the strong covalent bonds in its network structure.

Due to the weak forces between its atoms.

Because it is made of discrete molecules.

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the chemical formula for quartz, a mineral that exhibits network covalent bonding?

SiO2

CO2

CH4

H2O

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which of the following statements is true about quartz?

It is made of discrete molecules.

It is the most abundant mineral in many rocks.

It is the least common mineral in Earth's crust.

It has a low melting temperature.

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