Chapter 2 Earth Processes Day#3. Lesson plan
Enhancing AICE Marine Science Exam Success: Effective Strategies for Teaching Weathering, Erosion, and Sedimentation
As AICE Marine Science educators, our goal is to ensure that our students not only grasp fundamental concepts but also excel in their exams. Focusing on critical topics like weathering, erosion, and sedimentation can significantly boost their understanding and performance. In this blog post, we’ll explore effective strategies for teaching these concepts and provide detailed explanations to help your students distinguish between weathering and erosion, understand the main types of weathering and erosion, and grasp the process of sedimentation.
Objectives
- 2.2 Weathering, erosion, and sedimentation
- distinguish between weathering and erosion
- describe the three main types of weathering: chemical, physical and organic
- describe the four main types of erosion: by ice, water, wind and gravity
- describe sedimentation
Materials
- Lecture/Notes (PPT – slides 30 – 35 )
- Student Guided Notes
- Practical Activity 2.1: Investigating settlement speeds in sediments of varying sizes – page 54-55 (Coursebook)
Vocabulary
- Weathering: The wearing down or breaking of rocks through physical, chemical or organic means.
- Erosion: a natural process where material is worn away from the Earth’s surface and transported elsewhere
- Sedimentation: the deposition of suspended particles from water
- Deposition: a geological process where sediments, soil and rocks are added to a landform or land mass
Bellringer
- Bellringer#3
- Alternative: Describe how hydrothermal vents form.
Lesson Outline
Hook
- Greet students and introduce the lesson objectives.
- Provide a brief overview of the day’s topics.
- Discuss the importance of understanding weathering, erosion, and sedimentation in marine science.
Instruction
- Lecture/Notes
- Distinguishing Between Weathering and Erosion
- Weathering and erosion are often confused, but they refer to different processes:
- Weathering: The breakdown of rocks and minerals at their original location. Weathering can occur due to physical, chemical, or biological factors.
- Erosion: The movement of weathered materials from one location to another by natural forces such as water, wind, ice, or gravity.
- Weathering and erosion are often confused, but they refer to different processes:
- The Three Main Types of Weathering:
- Chemical Weathering
Involves the chemical breakdown of minerals within rocks. This type of weathering alters the rock’s chemical composition.
Common processes include oxidation, hydrolysis, and carbonation.
Example: Acid rain reacting with limestone to form calcium bicarbonate, which is easily dissolved in water. - Physical (Mechanical) Weathering
Involves the physical breakdown of rocks into smaller pieces without changing their chemical composition.
Common processes include freeze-thaw cycles, thermal expansion, and abrasion.
Example: Water seeps into cracks in rocks, freezes, expands, and eventually causes the rock to break apart. - Organic (Biological) Weathering
Involves the breakdown of rocks by living organisms.
Common processes include plant roots growing into cracks and animals burrowing.
Example: Tree roots growing into rock cracks, exerting pressure and causing the rock to fracture.
- Chemical Weathering
- The Four Main Types of Erosion
- Erosion by Ice
Glaciers move slowly over land, picking up rocks and soil and carving out valleys.
Example: The formation of U-shaped valleys by glacial movement. - Erosion by Water
Rivers, streams, and rainfall can carry away weathered materials.
Includes processes like river erosion, coastal erosion, and sheet erosion.
Example: The Grand Canyon was formed by the erosive action of the Colorado River. - Erosion by Wind
Wind can transport fine particles like sand and dust over long distances.
Common in arid and semi-arid regions.
Example: The formation of sand dunes on the beach. - Erosion by Gravity
The downward movement of rocks and soil due to gravity.
Includes processes like landslides, rockfalls, and soil creep.
Example: A landslide carrying large amounts of earth material down a slope.
- Erosion by Ice
- Understanding Sedimentation
- Sedimentation is the process by which eroded materials are deposited in new locations. It involves:
- Transport: Eroded particles are carried by agents like water, wind, ice, or gravity.
- Deposition: When the transporting medium loses energy, it drops the sediment it was carrying.
- Layer Formation: Over time, deposited sediments accumulate in layers, forming sedimentary rocks through compaction and cementation.
- Sedimentation is the process by which eroded materials are deposited in new locations. It involves:
- Distinguishing Between Weathering and Erosion


- Lab activity – Practical Activity 2.1: Investigating settlement speeds in sediments of varying sizes – page 54-55 (Coursebook)
- Students work in small groups
- perform the lab activity following the step-by-step description from the coursebook.
- students collect data and complete data table
- In their groups, students complete the evaluation and conclusion section of the practical activity and the reflection questions 1-2 page 55.
- Exit ticket
- If you opt to have students complete their notes using the Student Guided Notes format during your lecture, then use the bellringer as the exit ticket activity in class.
- If you opt to have students complete their notes using the Student Guided Notes format at home (homework), then use the following exit ticket activity:
- Students share conclusion of the Practical activity
By implementing these strategies and focusing on core concepts like weathering, erosion, and sedimentation, you can enhance your students’ comprehension and boost their performance in AICE Marine Science exams. Engaging lessons, practical experiences, and consistent practice with AICE-style questions will prepare your students for success.
Homework
- The sole homework task assigned to my students revolves around meticulously transcribing notes in the Student Guided Notes format. They meticulously replicate content by hand from the Lecture/Notes (PPT – slides 35 – 40 ) presentation.
- This approach ensures that during class time, while I continue to deliver lectures and expound on topics, students have their notes already compiled. Consequently, they can actively engage, ask questions, and delve deeper into understanding rather than merely being preoccupied with note-taking. This strategy efficiently liberates valuable class time, allowing for engaging activities and practice Cambridge style questions.


