TERM – 1ST TERM
WEEK ELEVEN
Class: Senior Secondary School 1
Age: 15 years
Duration: 40 minutes of 5 periods each
Date:
Subject: Geography
Topic: MAJOR LAND FORM FEATURES (MOUNTAINS)
SPECIFIC OBJECTIVES: At the end of the lesson, pupils should be able to
INSTRUCTIONAL TECHNIQUES: Identification, explanation, questions and answers,
demonstration, videos from source
INSTRUCTIONAL MATERIALS: Videos, loud speaker, textbook, pictures
INSTRUCTIONAL PROCEDURES
PERIOD 1-2
PRESENTATION |
TEACHER’S ACTIVITY |
STUDENT’S ACTIVITY |
STEP 1 INTRODUCTION |
The teacher introduces the mountains and identify the major types of mountains to the students. |
Students in groups mention different types of mountains. |
STEP 2 EXPLANATION |
Teacher explain the characteristics of each of the mountains and discusses the processes involved in their formation. |
Students in small groups highlight the characteristics of different types of mountain and describe the processes involved in the different mountain types |
STEP 3 DEMONSTRATIO N |
Teacher discusses the importance and effects of mountains to man |
Students in pairs justify the importance and effects of mountains to man. |
STEP 4 NOTE TAKING |
The teacher writes a summarized note on the board
|
The students copy the note in their books |
NOTE
MAJOR LAND FORM-FEATURES (MOUNTAINS)
A mountain is a large landform that rises prominently above its surroundings, typically having a peak or summit. Mountains are formed through various geological processes, and they exhibit diverse characteristics based on their origin and structure. The following are major types of mountains and their characteristics:
Characteristics: Parallel ridges and valleys, often with sharp peaks. Examples include the Himalayas and the Alps.
Mode of formation
The fold mountains results from tectonic plate collisions, where intense pressure causes the Earth's crust to buckle and fold.The Himalayas are a classic example, formed by the collision of the Indian and Eurasian plates.
Characteristics: Steep slopes on one side and gentler slopes on the other. The Sierra Nevada in the United States is an example.
Mode of formation
Fault-block mountains are develop when blocks of the Earth's crust are uplifted and tilted along faults.The Sierra Nevada in the United States is an example.
Characteristics: Rounded, dome-shaped summits. The Black Hills in South Dakota is an example.
Mode of formation
Dome mountains are formed by the upwelling of molten rock beneath the Earth's crust, creating a rounded or domed shape.The Black Hills in the United States are an example.
Characteristics: Conical shape, often with a crater at the summit. Examples include Mount St. Helens and Mount Fuji.
Mode of formation
Volcanic mountains are formed by the accumulation of volcanic material, such as lava and ash, from erupting volcanoes.Examples include the Andes in South America and the Cascade Range in North America.
Characteristics: Flat-topped with steep sides. The Drakensberg Mountains in South Africa exemplify this type.
Mode of formation
Plateau mountains are created from the erosion of plateaus, leaving behind isolated mountain blocks.The Colorado Plateau in the United States is an example.
EVALUATION: 1. What is a mountain?
CLASSWORK: As in evaluation
CONCLUSION: The teacher commends the students positively