Abstract
In
this lesson, students will discuss mountains and volcanoes
and explore connections between the different types of
each.
Purpose – Engagement of students in discovering the
different types of volcanoes and mountains and how they
form.
Objectives
Students
will be able to:
1. Identify mountains and volcanoes formed by collision boundaries on a
plate boundary map.
2. Identify mountains and volcanoes that are likely formed by other processes.
National Science
Education Standard:
CONTENT STANDARD D – Earth and Space Science
ENERGY IN THE EARTH SYSTEM
•
Earth systems have internal and external sources of energy, both of which
create heat. The sun is the major external source of energy. Two primary
sources of internal energy are the decay of radioactive isotopes and
the gravitational energy from the earth's original formation.
•
The outward transfer of earth's internal heat drives convection circulation
in the mantle that propels the plates comprising earth's surface across
the face of the globe.
THE ORIGIN AND EVOLUTION OF THE EARTH SYSTEM
• Interactions among the solid earth, the oceans, the atmosphere,
and organisms have resulted in the ongoing evolution of
the earth system. We can observe some changes such as earthquakes
and volcanic eruptions on a human time scale, but many
processes such as mountain building and plate movements
take place over hundreds of millions of years.
Teacher
Background
Earth
Science is not always straightforward. Although most
volcanoes
are formed at subduction zones, with volcanic
mountains forming on land and islands forming in the sea,
this is not always the case. Nor do all volcanoes look
alike. Some volcanoes are formed over “hot spots.” These
are places where the magma in the mantle spurt upward,
breaking through the crust. Volcanoes also vary their shape
depending upon the material that is extruded from them.
High viscosity magma, or ash eruptions, results in the
formation of strato-volcanoes. Low viscosity magma that
pours out of the volcano over a great area results in the
formation of shield volcanoes.
Mountains also vary. Many very large, tall mountain ranges
are the result of two continental plates colliding, However,
there are other ranges that are the result of faulting
in the earth. Parts of the plates are uplifted and form
mountain ranges. |