Lesson Notes By Weeks and Term - Senior Secondary 3

TERM – 1^ST TERM

WEEK ONE

Class: Senior Secondary School 3

Age: 17 years

Duration: 40 minutes of 5 periods each

Date:

Subject: Geography

Topic: VOLCANICITY

SPECIFIC OBJECTIVES: At the end of the lesson, pupils should be able to

1. Explain the meaning and processes of volcanicity
2. Identify regions of volcanic occurrences and explain why such regions are associated with earthquake
3. Describe the characteristics and forms of intrusive and extrusive features  of volcanicity
4. Analyse the effects of volcanicity on man and his environment

INSTRUCTIONAL TECHNIQUES: Identification, explanation, questions and answers,

demonstration, videos from source

INSTRUCTIONAL MATERIALS: Videos, loud speaker, textbook, pictures

INSTRUCTIONAL PROCEDURES

PERIOD 1-2

NOTE

VOLCANICITY

Volcanicity refers to the geological processes related to the formation and eruption of volcanoes. It involves the movement of molten rock (magma) from the Earth's mantle to the surface, resulting in volcanic activity.

 The major processes of volcanicity include:

1. Magma Generation: Magma, a molten mixture of rock, gases, and minerals, is formed within the Earth's mantle due to heat and pressure.
2. Magma Ascent: The magma rises through the Earth's crust, driven by buoyancy and pressure. It can move through cracks, fissures, or existing volcanic conduits.
3. Magma Chamber: The magma accumulates in a reservoir beneath the Earth's surface known as a magma chamber. This chamber acts as a temporary storage for magma before eruption.
4. Volcanic Eruption:When the pressure in the magma chamber exceeds the strength of the overlying rocks, volcanic eruption occurs. Magma, gases, and volcanic ash are expelled onto the Earth's surface through a vent or opening in the crust..

 Regions of volcanic occurrences

Volcanic activity is prevalent in specific regions known as volcanic arcs. Some notable areas include the Pacific Ring of Fire, which encircles the Pacific Ocean, and the East African Rift. Additionally, Iceland, Indonesia, and parts of Italy, such as Mount Vesuvius, are known for frequent volcanic activity.

The association between volcanic occurrences and earthquakes is primarily due to the dynamic nature of tectonic plate movements. The same geological forces that lead to magma generation and volcanic eruptions can also induce stress and strain on the Earth's crust, resulting in earthquakes.

Characteristics and forms of intrusive features of volcanicity

1. Batholiths: Batholiths are large, intrusive igneous rock masses that form deep within the Earth's crust. They represent the most massive and deeply seated type of intrusive rock bodies. Batholiths form from the cooling and solidification of magma beneath the Earth's surface over extended periods, typically millions of years.
2. Dikes: Dikes are tabular, sheet-like intrusive igneous rock formations that cut across existing rock layers vertically. They are formed by the intrusion of magma into pre-existing fractures and weaknesses in the Earth's crust. Dikes are often associated with volcanic activity. .
3. Sills: Sills are tabular, sheet-like intrusive igneous rock formations that parallel the existing rock layers. Similar to dikes, sills form through the intrusion of magma, but in this case, the magma spreads horizontally between existing rock layers. An

Characteristics and forms of extrusive features of volcanicity

1. Volcanic Cones: Volcanic cones, also known as stratovolcanoes or composite volcanoes, are conical-shaped mountains formed by the accumulation of erupted materials such as lava, ash, and volcanic rocks. These cones typically result from explosive eruptions that involve both lava flows and pyroclastic materials. The alternating layers of lava and pyroclastic deposits contribute to their characteristic cone shape..
2. Lava Plateaus: Lava plateaus are large, flat areas covered with solidified lava flows. They result from extensive volcanic activity that leads to the accumulation of successive lava layers. Lava plateaus form when fluid basaltic lava erupts from fissures or vents, spreading over a wide area and creating a thick layer of solidified basalt.
3. Pyroclastic Deposits: Pyroclastic deposits consist of fragmented volcanic materials ejected during explosive volcanic eruptions. These materials include ash, pumice, volcanic bombs, and lapilli. Pyroclastic deposits form when magma is fragmented into fine particles during explosive eruptions, and these particles are then transported and deposited by volcanic processes..

Effects of volcanicity on man and his environment

The following are effects of Volcanicity on Man and the Environment:

1.Volcanic soils are often rich in minerals, making them fertile for agriculture. Regions around volcanic areas may benefit from enhanced soil fertility, supporting crop growth.

2. Volcanic landscapes attract tourists, contributing to local economies. Volcanic features such as craters, lava fields, and hot springs can be popular attractions.
3. Volcanic regions often have geothermal resources, providing a sustainable and clean source of energy for power generation and heating.
4. Volcanic eruptions can pose threats to human settlements, causing destruction of infrastructure, homes, and farmland.
5. Volcanic ash and gases released during eruptions can pose health risks. Inhalation of volcanic ash can cause respiratory problems, and exposure to volcanic gases may be harmful.
6. Eruptions can lead to economic disruptions by damaging agriculture, disrupting transportation, and causing the evacuation of populated areas.
7. Large volcanic eruptions can release significant amounts of ash and gases into the atmosphere, affecting global climate. .

EVALUATION: 1. What is Volcanicity?

2. Describe the processes of volcanicity.
3. Identify the characteristics of intrusive and extrusive features of volcanicity.
4. Mention 5 effects of volcanicity on Man and his Environment

CLASSWORK: As in evaluation

CONCLUSION: The teacher commends the students positively