1. The lesson plan describes a science lesson on processes that shape the Earth's surface through weathering and soil erosion.
2. It includes objectives, materials, and procedures for the lesson involving a presentation, video, pictures and discussion of various types of weathering and erosion.
3. The lesson will teach students about physical and chemical weathering, different agents of erosion like water, wind and glaciers, and how these processes create landforms and affect soil.
Earth and life science- weathering erosion and deposition Project Presentatio...CloiePansoyTejoso
Weathering breaks down rocks into smaller pieces through mechanical and chemical processes. Erosion then transports these pieces and deposits them elsewhere. The main types of erosion are water erosion, wind erosion, and ice erosion. Water erosion occurs through running water that picks up and moves pieces downstream, potentially depositing them in locations like river deltas. Wind erosion moves small particles through sandstorms. Glacial ice erosion picks up and relocates rocks as glaciers move across the land.
The document summarizes the key processes involved in soil formation. It explains that soil is formed through the weathering of rock by various physical, chemical, and biological processes over long periods of time. Temperature and rainfall are identified as particularly important factors that influence soil formation rates and characteristics. The different types of weathering processes that break down rock into smaller particles that eventually become soil are also described in detail.
Weathering and soil erosion presentation.pptxFelcherLayugan
Rock weathering breaks down Earth's crust through physical and chemical processes. Physical weathering breaks rocks into smaller pieces through mechanical means like temperature changes, plant and animal activity, and abrasion. Chemical weathering alters the chemical composition of rocks through reactions with water, oxygen, carbon dioxide and acids. The rate of weathering depends on factors like climate, rock type, and exposure. Weathering produces sediments and soils that cover much of the Earth's surface.
The document discusses the formation of soil through weathering processes. It describes mechanical weathering which breaks down rock physically via frost wedging, pressure release, hydraulic action, salt crystal growth and thermal stress. It also describes chemical weathering which alters the molecular structure of rocks through dissolution, carbonation, hydration, hydrolysis and oxidation. The weathered rocks and minerals are broken down into clay, silt, sand and nutrients that combine with organic materials to form various soil types.
This document discusses weathering and soil formation. It describes two types of weathering - mechanical and chemical. Mechanical weathering breaks rocks into smaller pieces without changing their chemical composition, while chemical weathering alters the rocks' chemical makeup. Weathering occurs due to factors like temperature changes, frost action, abrasion, and acids. Over time, weathering breaks rocks down into soil. Soil provides nutrients for plants and animals and is important for life. The document also examines different types of soil like residual and transported soil and how soil composition varies by location.
This document discusses weathering and soil formation. It describes two types of weathering - mechanical and chemical - and their causes such as temperature changes, frost action, oxidation, and acids. Mechanical weathering breaks rocks into smaller pieces without changing their chemical composition, while chemical weathering alters the rocks' minerals. Over time, weathered rocks break down into soil. Factors like climate, rock type, and time influence soil formation, which results in distinct layers or horizons of topsoil, subsoil, and partially weathered parent material.
Earth and life science- weathering erosion and deposition Project Presentatio...CloiePansoyTejoso
Weathering breaks down rocks into smaller pieces through mechanical and chemical processes. Erosion then transports these pieces and deposits them elsewhere. The main types of erosion are water erosion, wind erosion, and ice erosion. Water erosion occurs through running water that picks up and moves pieces downstream, potentially depositing them in locations like river deltas. Wind erosion moves small particles through sandstorms. Glacial ice erosion picks up and relocates rocks as glaciers move across the land.
The document summarizes the key processes involved in soil formation. It explains that soil is formed through the weathering of rock by various physical, chemical, and biological processes over long periods of time. Temperature and rainfall are identified as particularly important factors that influence soil formation rates and characteristics. The different types of weathering processes that break down rock into smaller particles that eventually become soil are also described in detail.
Weathering and soil erosion presentation.pptxFelcherLayugan
Rock weathering breaks down Earth's crust through physical and chemical processes. Physical weathering breaks rocks into smaller pieces through mechanical means like temperature changes, plant and animal activity, and abrasion. Chemical weathering alters the chemical composition of rocks through reactions with water, oxygen, carbon dioxide and acids. The rate of weathering depends on factors like climate, rock type, and exposure. Weathering produces sediments and soils that cover much of the Earth's surface.
The document discusses the formation of soil through weathering processes. It describes mechanical weathering which breaks down rock physically via frost wedging, pressure release, hydraulic action, salt crystal growth and thermal stress. It also describes chemical weathering which alters the molecular structure of rocks through dissolution, carbonation, hydration, hydrolysis and oxidation. The weathered rocks and minerals are broken down into clay, silt, sand and nutrients that combine with organic materials to form various soil types.
This document discusses weathering and soil formation. It describes two types of weathering - mechanical and chemical. Mechanical weathering breaks rocks into smaller pieces without changing their chemical composition, while chemical weathering alters the rocks' chemical makeup. Weathering occurs due to factors like temperature changes, frost action, abrasion, and acids. Over time, weathering breaks rocks down into soil. Soil provides nutrients for plants and animals and is important for life. The document also examines different types of soil like residual and transported soil and how soil composition varies by location.
This document discusses weathering and soil formation. It describes two types of weathering - mechanical and chemical - and their causes such as temperature changes, frost action, oxidation, and acids. Mechanical weathering breaks rocks into smaller pieces without changing their chemical composition, while chemical weathering alters the rocks' minerals. Over time, weathered rocks break down into soil. Factors like climate, rock type, and time influence soil formation, which results in distinct layers or horizons of topsoil, subsoil, and partially weathered parent material.
lessons in Weathering of Grade five.pptxNeilDeclaro1
Mechanical and chemical weathering break rocks down into sediments and soil. Mechanical weathering involves physical breakdown through forces like frost wedging when water freezes in cracks. Chemical weathering changes the rocks' composition through acids. Weathering is important for producing soil but excessive erosion from agents like water and wind can harm the environment if not prevented through measures like planting vegetation.
Music In Mental Health This Is A Wonderful Ppt22wj5a0130
This document discusses weathering and soil formation. It describes two types of weathering - mechanical and chemical - and their causes such as temperature changes, frost action, oxidation, and acids. Mechanical weathering breaks rocks into smaller pieces without changing their chemical composition, while chemical weathering alters the rocks' minerals. Over time, weathered rocks break down into soil. Factors like climate, rock type, and time influence soil formation, which results in distinct layers or horizons of topsoil, subsoil, and partially weathered parent material.
This document provides an overview of Earth's structure and the geological processes that shape its surface. It discusses how Earth is layered with an inner and outer core, mantle, and crust. Plate tectonics cause earthquakes and volcanoes at plate boundaries. Weathering and erosion gradually break down rock at the surface through mechanical and chemical means. Minerals and rocks can be identified by their properties and how they form.
This document provides an overview of Earth's structure and the geological processes that shape its surface. It discusses how Earth is layered with an inner and outer core, mantle, and crust. Plate tectonics cause earthquakes and volcanoes at plate boundaries. Weathering and erosion gradually break down rock at the surface through mechanical and chemical means. Minerals and rocks can be identified by their properties and how they form.
This document discusses exogenetic (external) geologic processes and the landforms they create. It describes three types of weathering - mechanical, chemical, and biological - and how they break down rock material. Mechanical weathering is caused by temperature changes, frost action, crystal growth, and more. Chemical weathering is aided by water and acids. Biological weathering occurs when roots break apart rocks. The document also discusses mass movements of weathered material due to gravity, like soil creep, landslides, and mudslides, as well as erosion from various agents.
This document discusses various earth processes including weathering, mass wasting, and soil erosion. It defines weathering as the breakdown of rocks near the earth's surface due to elements like temperature, rainfall, and frost. Weathering occurs through physical processes like exfoliation or chemical processes like oxidation. Mass wasting is the downward movement of rock and soil under gravity, and includes different types of movement like falls, slides, and flows. Soil erosion is the removal of soil faster than its replacement, and can occur through various agents like wind, water, or human activities.
Chemical weathering is more useful in soil formation than mechanical weathering because:
- Chemical weathering changes the minerals in rocks and causes new substances to form. This releases nutrients from the rocks that plants can use.
- Mechanical weathering only breaks rocks into smaller pieces through physical processes like temperature changes, abrasion, etc. but does not release as many nutrients.
- The new substances formed during chemical weathering like carbonic acid help dissolve more rocks and release more nutrients into the soil over time compared to mechanical weathering alone.
- Released nutrients are important for plant growth. As more plants grow, they add more organic matter to the soil through their remains. Organic matter is a key component of healthy
Mountains are landforms that rise steeply above surrounding land. They form through various geological processes such as volcanic eruptions, uplifting of the Earth's crust, erosion, and folding of layers. The highest mountain is Mount Everest at 8,849 meters tall. Mountains have varying climates depending on elevation, with colder temperatures and less oxygen at higher elevations. The main types of mountains include volcanic, dome, erosional, fault-block, and folded mountains.
The document summarizes the processes of weathering, erosion, and deposition. It describes how weathering breaks down rocks through mechanical and chemical processes. Erosion then transports this weathered material, which is deposited in new locations through various agents such as running water, glaciers, wind, and ocean waves. This forms new landforms and shapes the Earth's surface over time through the continuous weathering, erosion, and deposition cycle.
This document discusses weathering and erosion. It defines weathering as the breakdown and decomposition of rocks near the Earth's surface. Weathering occurs through various processes including expansion/contraction from temperature changes, freezing and thawing of water in cracks, and chemical breakdown. Erosion is defined as the removal and transport of weathered materials. The key influences on weathering are temperature, rainfall, and biological factors like plant and animal activity. Weathering and erosion can have both positive impacts through soil formation and raw materials, and negative impacts like flood damage.
Weathering is the breakdown of rocks at the Earth's surface by processes including physical and chemical weathering. Physical weathering breaks rocks apart through temperature changes causing expansion and contraction. It includes freeze-thaw weathering in cold regions and exfoliation in uplifted areas. Chemical weathering involves reactions between rock minerals and water, sometimes aided by carbon dioxide and acid rain, forming new minerals and soluble compounds. Together these processes break down bedrock into sediment.
This document discusses various exogenic and endogenic geological processes that shape the Earth's surface and interior. It describes weathering processes like physical weathering caused by temperature fluctuations, plants, and abrasion that break down rock. It also discusses chemical weathering processes like hydrolysis, carbonation, and oxidation. Erosion by water and wind then transport weathered material. These surface processes interact with sub-surface processes like plate tectonics and magmatism to continually reshape the Earth's surface through folding, faulting, earthquakes, and volcanism over millions of years. Together exogenic and endogenic processes create diverse landforms and landscapes.
1) Soil is formed from two main components - tiny pieces of weathered rock and humus, which is composed of decomposed dead plants and animals.
2) Rocks are weathered into smaller pieces through natural forces like water, wind, freezing and thawing. Over long periods of time, these break rocks down from boulders into soil.
3) Humus is formed as bacteria, fungi and invertebrates decompose dead organic matter through a process of rotting and decay. This decomposition of plants and animals is what creates the dark, nutrient-rich organic component of soil.
This document provides information about igneous, sedimentary, and metamorphic rocks. It begins with the lesson objectives of classifying rocks into these three categories. It then discusses each rock type in detail, including their formation processes and examples. Various diagrams illustrate concepts like the rock cycle and types of metamorphism. Activities are included to help students understand rock identification and transformations through the rock cycle.
The document discusses various exogenic (surface) processes including weathering, mass wasting, and soil erosion. It describes three main types of weathering - physical, chemical, and biotic weathering. Physical weathering breaks rocks into smaller pieces through mechanical processes like heating/cooling or frost action without changing the chemical composition. Chemical weathering alters the chemical makeup of rocks through oxidation, carbonation, hydration, or solution. Biotic weathering is caused by living organisms through root growth, burrowing, or human activities. Mass wasting and soil erosion are also exogenic processes that transport weathered material downslope or remove soil faster than replacement through water, wind, ice, or gravity.
The document discusses various exogenic (surface) processes including weathering, mass wasting, and soil erosion. It describes three main types of weathering - physical, chemical, and biotic weathering. Physical weathering breaks rocks into smaller pieces through mechanical processes like heating/cooling or frost action without changing the chemical composition. Chemical weathering alters the chemical makeup of rocks through oxidation, carbonation, hydration, or solution. Biotic weathering is caused by living organisms through root growth, burrowing, or human activities. Mass wasting and soil erosion are also exogenic processes that transport weathered material downslope or remove soil faster than replacement through water, wind, ice, or gravity.
This document discusses various exogenous (external) geological processes that shape the Earth's surface features. It describes weathering as the physical and chemical breakdown of rocks, including frost wedging, salt crystal growth, and hydrolysis. Erosion is defined as the removal and transport of weathered materials by agents like water, wind, and ice. Mass movement involves the downslope transport of soil and rock due to gravity, including processes like creep, landslides, and rockfalls.
Rocks vary in size, shape, and texture due to weathering and erosion over hundreds of years. Weathering breaks rocks into smaller pieces through mechanical and chemical processes. Mechanical weathering is caused by forces like water, wind, ice, and plants. Chemical weathering occurs when acids from water and carbon dioxide dissolve minerals. Erosion then transports these sediment particles to new locations through agents like wind, water, and animals. This constant weathering and erosion gradually reshapes the landscape over time.
This document discusses a lecture on weathering and erosion given by Dr. Shahid Ullah. It covers the main topics of the lecture including definitions of weathering and the processes involved, physical and chemical agents that cause weathering, factors affecting the rate of weathering, the products of weathering, erosion and factors influencing erosion rates. The document provides detailed explanations and examples of various weathering and erosion concepts.
This lesson teaches students about adverbs of intensity and frequency. It defines adverbs of intensity as words that describe the degree or extent to which something is done or exists. Examples given are "very", "quite", and "too". Adverbs of frequency describe how often something occurs, and examples provided are "always", "sometimes", and "never". The lesson contains activities where students identify these adverbs in sentences and use them correctly in their own writing. Students learn to recognize and apply these adverb types to compose clear sentences.
This self-learning module provides instruction on interactions among living and non-living things in intertidal zones and estuarine ecosystems. It is divided into three lessons that cover abiotic factors, biotic factors, and feeding relationships. The lessons define key concepts and provide examples of organisms found in different habitats within intertidal zones and estuaries. Students are expected to identify abiotic and biotic factors, explain their effects, and demonstrate understanding of food chains and webs after completing the module.
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lessons in Weathering of Grade five.pptxNeilDeclaro1
Mechanical and chemical weathering break rocks down into sediments and soil. Mechanical weathering involves physical breakdown through forces like frost wedging when water freezes in cracks. Chemical weathering changes the rocks' composition through acids. Weathering is important for producing soil but excessive erosion from agents like water and wind can harm the environment if not prevented through measures like planting vegetation.
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This document discusses weathering and soil formation. It describes two types of weathering - mechanical and chemical - and their causes such as temperature changes, frost action, oxidation, and acids. Mechanical weathering breaks rocks into smaller pieces without changing their chemical composition, while chemical weathering alters the rocks' minerals. Over time, weathered rocks break down into soil. Factors like climate, rock type, and time influence soil formation, which results in distinct layers or horizons of topsoil, subsoil, and partially weathered parent material.
This document provides an overview of Earth's structure and the geological processes that shape its surface. It discusses how Earth is layered with an inner and outer core, mantle, and crust. Plate tectonics cause earthquakes and volcanoes at plate boundaries. Weathering and erosion gradually break down rock at the surface through mechanical and chemical means. Minerals and rocks can be identified by their properties and how they form.
This document provides an overview of Earth's structure and the geological processes that shape its surface. It discusses how Earth is layered with an inner and outer core, mantle, and crust. Plate tectonics cause earthquakes and volcanoes at plate boundaries. Weathering and erosion gradually break down rock at the surface through mechanical and chemical means. Minerals and rocks can be identified by their properties and how they form.
This document discusses exogenetic (external) geologic processes and the landforms they create. It describes three types of weathering - mechanical, chemical, and biological - and how they break down rock material. Mechanical weathering is caused by temperature changes, frost action, crystal growth, and more. Chemical weathering is aided by water and acids. Biological weathering occurs when roots break apart rocks. The document also discusses mass movements of weathered material due to gravity, like soil creep, landslides, and mudslides, as well as erosion from various agents.
This document discusses various earth processes including weathering, mass wasting, and soil erosion. It defines weathering as the breakdown of rocks near the earth's surface due to elements like temperature, rainfall, and frost. Weathering occurs through physical processes like exfoliation or chemical processes like oxidation. Mass wasting is the downward movement of rock and soil under gravity, and includes different types of movement like falls, slides, and flows. Soil erosion is the removal of soil faster than its replacement, and can occur through various agents like wind, water, or human activities.
Chemical weathering is more useful in soil formation than mechanical weathering because:
- Chemical weathering changes the minerals in rocks and causes new substances to form. This releases nutrients from the rocks that plants can use.
- Mechanical weathering only breaks rocks into smaller pieces through physical processes like temperature changes, abrasion, etc. but does not release as many nutrients.
- The new substances formed during chemical weathering like carbonic acid help dissolve more rocks and release more nutrients into the soil over time compared to mechanical weathering alone.
- Released nutrients are important for plant growth. As more plants grow, they add more organic matter to the soil through their remains. Organic matter is a key component of healthy
Mountains are landforms that rise steeply above surrounding land. They form through various geological processes such as volcanic eruptions, uplifting of the Earth's crust, erosion, and folding of layers. The highest mountain is Mount Everest at 8,849 meters tall. Mountains have varying climates depending on elevation, with colder temperatures and less oxygen at higher elevations. The main types of mountains include volcanic, dome, erosional, fault-block, and folded mountains.
The document summarizes the processes of weathering, erosion, and deposition. It describes how weathering breaks down rocks through mechanical and chemical processes. Erosion then transports this weathered material, which is deposited in new locations through various agents such as running water, glaciers, wind, and ocean waves. This forms new landforms and shapes the Earth's surface over time through the continuous weathering, erosion, and deposition cycle.
This document discusses weathering and erosion. It defines weathering as the breakdown and decomposition of rocks near the Earth's surface. Weathering occurs through various processes including expansion/contraction from temperature changes, freezing and thawing of water in cracks, and chemical breakdown. Erosion is defined as the removal and transport of weathered materials. The key influences on weathering are temperature, rainfall, and biological factors like plant and animal activity. Weathering and erosion can have both positive impacts through soil formation and raw materials, and negative impacts like flood damage.
Weathering is the breakdown of rocks at the Earth's surface by processes including physical and chemical weathering. Physical weathering breaks rocks apart through temperature changes causing expansion and contraction. It includes freeze-thaw weathering in cold regions and exfoliation in uplifted areas. Chemical weathering involves reactions between rock minerals and water, sometimes aided by carbon dioxide and acid rain, forming new minerals and soluble compounds. Together these processes break down bedrock into sediment.
This document discusses various exogenic and endogenic geological processes that shape the Earth's surface and interior. It describes weathering processes like physical weathering caused by temperature fluctuations, plants, and abrasion that break down rock. It also discusses chemical weathering processes like hydrolysis, carbonation, and oxidation. Erosion by water and wind then transport weathered material. These surface processes interact with sub-surface processes like plate tectonics and magmatism to continually reshape the Earth's surface through folding, faulting, earthquakes, and volcanism over millions of years. Together exogenic and endogenic processes create diverse landforms and landscapes.
1) Soil is formed from two main components - tiny pieces of weathered rock and humus, which is composed of decomposed dead plants and animals.
2) Rocks are weathered into smaller pieces through natural forces like water, wind, freezing and thawing. Over long periods of time, these break rocks down from boulders into soil.
3) Humus is formed as bacteria, fungi and invertebrates decompose dead organic matter through a process of rotting and decay. This decomposition of plants and animals is what creates the dark, nutrient-rich organic component of soil.
This document provides information about igneous, sedimentary, and metamorphic rocks. It begins with the lesson objectives of classifying rocks into these three categories. It then discusses each rock type in detail, including their formation processes and examples. Various diagrams illustrate concepts like the rock cycle and types of metamorphism. Activities are included to help students understand rock identification and transformations through the rock cycle.
The document discusses various exogenic (surface) processes including weathering, mass wasting, and soil erosion. It describes three main types of weathering - physical, chemical, and biotic weathering. Physical weathering breaks rocks into smaller pieces through mechanical processes like heating/cooling or frost action without changing the chemical composition. Chemical weathering alters the chemical makeup of rocks through oxidation, carbonation, hydration, or solution. Biotic weathering is caused by living organisms through root growth, burrowing, or human activities. Mass wasting and soil erosion are also exogenic processes that transport weathered material downslope or remove soil faster than replacement through water, wind, ice, or gravity.
The document discusses various exogenic (surface) processes including weathering, mass wasting, and soil erosion. It describes three main types of weathering - physical, chemical, and biotic weathering. Physical weathering breaks rocks into smaller pieces through mechanical processes like heating/cooling or frost action without changing the chemical composition. Chemical weathering alters the chemical makeup of rocks through oxidation, carbonation, hydration, or solution. Biotic weathering is caused by living organisms through root growth, burrowing, or human activities. Mass wasting and soil erosion are also exogenic processes that transport weathered material downslope or remove soil faster than replacement through water, wind, ice, or gravity.
This document discusses various exogenous (external) geological processes that shape the Earth's surface features. It describes weathering as the physical and chemical breakdown of rocks, including frost wedging, salt crystal growth, and hydrolysis. Erosion is defined as the removal and transport of weathered materials by agents like water, wind, and ice. Mass movement involves the downslope transport of soil and rock due to gravity, including processes like creep, landslides, and rockfalls.
Rocks vary in size, shape, and texture due to weathering and erosion over hundreds of years. Weathering breaks rocks into smaller pieces through mechanical and chemical processes. Mechanical weathering is caused by forces like water, wind, ice, and plants. Chemical weathering occurs when acids from water and carbon dioxide dissolve minerals. Erosion then transports these sediment particles to new locations through agents like wind, water, and animals. This constant weathering and erosion gradually reshapes the landscape over time.
This document discusses a lecture on weathering and erosion given by Dr. Shahid Ullah. It covers the main topics of the lecture including definitions of weathering and the processes involved, physical and chemical agents that cause weathering, factors affecting the rate of weathering, the products of weathering, erosion and factors influencing erosion rates. The document provides detailed explanations and examples of various weathering and erosion concepts.
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This lesson teaches students about adverbs of intensity and frequency. It defines adverbs of intensity as words that describe the degree or extent to which something is done or exists. Examples given are "very", "quite", and "too". Adverbs of frequency describe how often something occurs, and examples provided are "always", "sometimes", and "never". The lesson contains activities where students identify these adverbs in sentences and use them correctly in their own writing. Students learn to recognize and apply these adverb types to compose clear sentences.
This self-learning module provides instruction on interactions among living and non-living things in intertidal zones and estuarine ecosystems. It is divided into three lessons that cover abiotic factors, biotic factors, and feeding relationships. The lessons define key concepts and provide examples of organisms found in different habitats within intertidal zones and estuaries. Students are expected to identify abiotic and biotic factors, explain their effects, and demonstrate understanding of food chains and webs after completing the module.
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1. Detailed Lesson Plan
In Science Grade V
Knessa Marie C. Orbesido January 27, 2020
BEED Date of Demonstration
Jasper Ocampo 8:00-9:00 am
Critic Teacher Time of Demonstration
I. Objectives
At the end of the lesson the student will be able to:
a. Describe how rock turn into soil
b. Investigate extent of soil erosion in the community
c. Communicate the data collected from the investigation on soil erosion
d. To understand the effects of erosion in shaping our earths surface
II. Subject Matter
Topic/Lesson: Processes that Shape of Earth’s surface: Weathering and Soil Erosion
1. Science Journey 5, Ryan Bautista, Alvin L. Banlaygas, Carmencita S. Bugayan, Liamie B.
Raposa. Copyright 2016 pp 297-301
2. Science in Our World Norma M. Abracia, Edd. D., Evelyn T. Sarte , Ed. D, Ednaliza R.
Garcia, Mary Jean G. dela Cruz, Harold A. Arrazada, Rosemarie S. Punsalan
Ritche Aldwin dc. Tomelde, Eliza A. Lopez.Copyright 2014 pp 200-222
3. https://www.britannica.com/science/erosion-geology
4. https://courses.lumenlearning.com/wmopen-geology/chapter/outcome-weathering-
and-erosion/
5. https://www.generationgenius.com/weathering-erosion-and-deposition-for-kids/
Materials:
Picture (presented via projector), Video clip
III. Procedure
Teachers Activity Students Activity
A. Preliminaries
1. Prayer and Greetings.
Okay class, please stand for a prayer.
Our Father in heaven, hallowed be your
name. Your kingdom come, your will be
done, on earth as it is in heaven. Give us
this day our daily bread, and forgive us
our debts, as we also have forgiven our
debtors. And lead us not into temptation,
but deliver us from evil. Amen.
Students Activity
Our Father in heaven, hallowed be
your name. Your kingdom come,
your will be done, on earth as it is
in heaven. Give us this day our daily
bread, and forgive us our debts, as
we also have forgiven our debtors.
And lead us not into temptation,
but deliver us from evil. Amen.
2. Good morning Class
2. Attendance
May I please ask someone from each
group to give me the names of those
students that were absent?
Thank you.
B. New Lesson
1. Motivation
I have here a picture of the
Kapurpurawan Rock Formation in Burgos,
Ilocos Norte. Have you been there? What
other beautiful places in the Philippines
have you been to?
Class what do you see while you were in
an island beach resort?
Yes, you noticed as well. Now, what do
you think why are those rock has
different forms?
You got an idea.
2. Presentation
Class our lesson for today is all about the:
Processes that Shape of Earth’s surface:
Weathering and Soil Erosion
2.1 Spring board
Now, I have here a video clip entitled:
Weathering. I want you to pay attention
as you watch the video. Understood?
Based on the video what are factors that
cause weathering?
Do you agree that human activities affect
also affects weathering?
Very good!
Good morning Teacher Knessa.
Yes Teacher Knessa, and I have
been with other places.
There are different rock formations
that we can see.
Because of the waves that is hitting
the rock.
Yes Teacher Knessa.
The factors that causes weathering
are water, ice, wind, plants, heating
and cooling
Yes Teacher Knessa ,because
humans are also doing mining and
they dig the soil to build
infrastructure.
3. Alright, today I am going to present to
you not only factors that affects
weathering, but also learning what are
different forms of weathering and their
components.
Okay class I have here a sample picture of
a rock. What can you observe?
Now, weathering is a process where a
rock breaks down into smaller pieces into
the earth’s surface. Weathering may be
physical or chemical.
Physical weathering, also called
mechanical weathering breaks down
rocks without changing their chemical
composition. Physical weathering
involves the breakdown of rocks and
soils through direct contact with
atmospheric conditions, such as heat,
water, ice and pressure. Mechanical
or physical weathering breaks rock
into smaller pieces. These smaller
pieces are just like the bigger rock,
just smaller. That means that the rock
has change physically without
changing its composition. The smaller
pieces have the same minerals, in just
the same portions as the original
rock. During the day, the other layer
of a rock is hot while the center is
cold. So the other layer of the rock
expands slightly. At night, when the
temperature drops the outer layer
cools faster than its center and
contracts slightly. After sometime,
the outer layer of the rock cracks and
breaks off.
In very cold areas, weathering
involves water. When water in the
cracks of the rocks freezes, it
expands. This expansion widens the
cracks. After sometime, the rocks are
broken down into pieces this process
Teacher Knessa I can see that the
rock breaks into pieces.
4. is known as ice wedging.
Ice wedging is common in mountain areas
where the temperature is around the
freezing point of water. Ice wedging
breaks apart so much rock that large piles
of broken rock are seen at the base of a
hillside. Ice wedging is common in Earth’s
polar regions and mid altitudes and also
at higher elevations
Roots grow into cracks where water and
nutrients might be. As the roots grow,
they wedge the rocks apart. Plants and
animals can do the work of mechanical
weathering This could happen slowly as a
plant’s roots grow into a crack or fracture
in rock and gradually grow larger,
wedging open the crack. Burrowing
animals can also break apart rock as they
dig for food or to make living spaces for
themselves.
Chemical weathering involves chemical
reactions. Remember that the most
common minerals in Earth’s crust are the
silicate minerals. Many silicate minerals
form in igneous or metamorphic rocks.
The minerals that form at the highest
temperatures and pressures are the least
stable at the surface. There are many
types of chemical weathering because
there are many agents of chemical
weathering. Water is the most important
agent of chemical weathering. Two other
important agents of chemical weathering
are carbon dioxide and oxygen.
Rain is naturally slightly acidic as carbon
dioxide dissolves in it. Some rocks such as
limestone have minerals in them that
react with the acidic rain water. The
chemical reactions makes the rock
weathered. Chemical weathering is
different from mechanical weathering
because the rocks Changes, not just in
size of pieces, but in composition. That is
one type of mineral changes into a
5. different mineral. Chemical weathering
works through chemical reactions that
cause the change in the minerals
When the fossil fuel as coal and gasoline
are burnt more acidic gases are released
into the air. This makes rainwater more
acidic. This is known as acid rain. Acid rain
speeds up the chemical weathering.
Building and stonework are damaged as a
result.
During weathering, large rocks are broken
down into smaller and movable pieces.
Then, they are broken down further
through erosion.
Erosion is the process of weathering
down and removal of rocks and soil
materials by natural agents, such as
running water, waves, glaciers, and wind.
It is also a process wherein the removals
of surface material from the earths crust
primarily soil and rock debris and the
transportation of the eroded materials by
natural agents such as water or wind.
Erosion will often occur after a rock has
been disintegrated or altered through
weathering. Weathered rock material will
be removed from its original sites and
transported away by natural agents
There are many factors that are affecting
soil erosion. The agents of soil erosion are
the same as the agents of all types of
erosion: water, wind, ice, or gravity and
waves. How does Gravity cause Erosion?
Erosion that happens as gravity moves
materials down slope. Examples are rock
slide, mudslide and land slide.
Glacier is a large mass of ice and snow
moving on land under its own weight. As
glaciers pass over land, they erode it,
changing features on the surface then
carry eroded material along and deposit it
somewhere else.
There are 2 types of glaciers: Continental
and Valley Glaciers
6. Continental Glacier is a glacier that covers
much of a continent or large island. These
glaciers can flow out in all directions,
spreading out like pancake batter in a pan
Valley Glacier is a long, narrow glacier
that forms when snow and ice build up
high in a mountain valley. The sides of the
mountains keep these glaciers from
spreading out in all directions
The two process by which glaciers erode
the land are plucking and abrasion
As a glacier flows over the land, it picks
up rocks in a process called plucking,
abrasion occurs as it scratches the
bedrock
Wind by itself is the weakest agent of
erosion, however, it can be a powerful
force in shaping the land areas where
there are few plants to hold the soil in
place
Abrasion by wind-carried sand can polish
rock, but causes little erosion
What are some landforms created by
wind erosion?
Sand dunes are mounds of sediment
drifted by the wind.
Loess are fine, wind blown sediment like
silt and clay which help to form fertile soil
and create valuable farmlands.
Running water is the leading cause of soil
erosion, because water is abundant and
has a lot of power. Through erosion, a
river creates valleys, water falls, flood
plains, and other landforms
Through erosion, a river creates valleys,
water falls, flood plains, and other
landforms. Deposition of sediments
creates landforms such as deltas and also
adds soil to a river’s flood plain. A delta is
sediment that are deposited where a
river flows into an ocean or lake building
up a landform
How do waves contribute to Erosion?
7. The energy in waves comes from wind
that blows across the water’s surface.
Waves shape the coast through erosion
by breaking down rock and transporting
sand and other sediment. Waves shape a
coast when they deposit sediment,
forming coastal features such as beaches
Here are some examples on how we can
lessen our soil erosion
Plant trees to prevent landslides.
Tree roots are powerful tools when soil is
too eroded or steep to plant. Plant native
trees on steep slopes and riverbanks to
reduce soil loss
Keep in mind that older trees will be
more effective at preventing landslides
than new saplings. It may take some time
before your tree develops roots that are
strong enough.
Reduce tillage.
Deep, frequent tillage creates a layer of
compact soil vulnerable to water erosion,
topped by loose soil easily removed by
wind.[
Consider a zero-tillage approach using a
coulter or other deep planting device
hese conservation tillage techniques also
reduce the amount of vehicle traffic, and
therefore soil compaction.
Avoid soil compaction.
When people, animals, or machines
travel over soil, they press it down,
compacting the soil into a dense layer.
Since there is less space between dirt
particles in compacted soil, water has a
hard time draining through, and carries
soil on the surface downhill instead. Walk
on paving stones or cleared paths instead
of trampling the soil, especially when it is
wet.
Build retaining walls.
Badly eroded slopes will continue to
8. collapse downhill until they are stabilized.
A retaining wall at the base of the slope
will block the soil and slow down the
collapse. This gives grass or other plants
time to grow and help the soil hold
together.
Reduce watering if possible.
Over-watering your garden can speed up
erosion by washing away soil. Use less
water if you can, or install a drip irrigation
system. Since a drip system only delivers
small amounts of water at a time, there is
no water flooding across the surface to
carry topsoil.
3. Discussion
Now, let me see if you got my
presentation.
a. What are the two types of
weathering?
Yes, you are right! According to the book
weathering may be physical or chemical.
b. What is mechanical weathering?
Yes, you are right mechanical or
physical weathering breaks rock into
smaller pieces. These smaller pieces
are just like the bigger rock, just
smaller. That means that the rock has
change physically without changing
its composition. The smaller pieces
have the same minerals, in just the
same portions as the original rock.
c. What is chemical weathering?
Very good, chemical weathering is
different from mechanical weathering
because the rocks Changes, not just
in size of pieces, but in composition.
That is one type of mineral changes
Teacher, the two types of
weathering are physical and
chemical weathering.
Teacher mechanical weathering
breaks a rock into smaller pieces
without changing their
composition.
Teacher chemical weathering
involves chemical reaction that
make the rock weathered
9. into a different mineral. Chemical
weathering works through chemical
reactions that cause the change in
the minerals.
d. What do call when the rock is
breaking apart in areas with
temperature that freezing in the day
and night
Yes, you are correct, ice wedging
breaks apart so much rock that large
piles of broken rock are seen at the
base of a hillside. Ice wedging is
common in Earth’s polar regions and
mid altitudes and also at higher
elevations.
e. What is the process of removal of
surface material from the earth’s
crust?
Yes you are correct. Erosion process
wherein the removals of surface
material from the earths crust
primarily soil and rock debris and the
transportation of the eroded
materials by natural agents such as
water or wind. Erosion will often
occur after a rock has been
disintegrated or altered through
weathering
f. As student can you contribute to
avoid soil erosion?
You are correct you can help in planting
trees because trees can hold the soil from
being eroded.
4. Enrichment
Class I have here some pictures that
shows the different activities that causes
erosion. Identify the pictures that are
Teacher the rock breaking apart in
cold area is called ice wedging
Teacher the process of removal of
surface material from the earth’s
crust called erosion
Teacher that things that I can
contribute to avoid soil erosion is
by helping in planting trees.
Activities that do not cause erosion.
10. showing activities that is NOT causing soil
erosion and identify the activities that
causes erosion.
Now, I am going to pick up six students
who will go to the board identify each
picture.
Very good!
Activities that cause erosion.
11. 5. Application
On a clean sheet of paper I want you to
write on a clean sheet of paper I want to
answer this question.
The picture shows a large rock breaking
apart. Which of these is MOST likely
making the rock break apart? Explain
your answer.
Okay for those who are finish kindly raise
your hand.
Are you ready to give your answer?
Okay class kindly read that have you
written on your paper.
Very good. As the roots grow, they
wedge the rocks apart. In order to get
water and nutrients to sustain their
Yes Teacher Knessa.
Teacher the rock is breaking apart
because of the roots of the trees
breaks down the rock where they
get where water and nutrients.
12. growth.
6. Valuing
What is the positive effect of soil erosion?
Very good however class that too much
soil erosion can also cause the soil to
erode and strip the land that can make
bad land for farming
Have you ever watch news about
landslide?
And the worst part of it was many houses
were destroyed.
7. Evaluation
Okay class, please get a ½ sheet of pad
paper and answer the following activity.
A. Multiple choices.
1. The breaking down of rocks into
smaller particles
such as sand and pebbles is:
A. weathering
B. erosion
C. done only by animals
2. Weathering of rocks which does
involve the action of chemicals is:
A. erosion
B. physical weathering
C. chemical weathering
3. Water can break down rocks
because:
A. water carries strong acids that erode
rocks
B. water takes up less space when it
freezes and rocks collapse inward
C. water expands when it freezes in
cracks in rocks
Teacher the positive effect of soil
erosion is allow new soil to be
scattered on a dead soil.
Yes Teacher Knessa.
B. Erosion
C. Chemical weathering
A. water carries strong acids that
erode rocks
13. 3. What is formed when gases such as
carbon dioxide, sulphur dioxide and
nitrogen oxides mix with rain?
A. erosion
B. acid rain
C. lichens
4. City council regulations ban the planting
of certain trees near buildings because:
A. tree roots can damage and break down
concrete
B. the tree sap is poisonous to humans
C. trees create shade and the
temperature extremes can break
concrete
B. Identification
Answer the following question and
get the answer
inside the box.
Deep freeze Ice Wedging
Physical weathering Weathering
Erosion Glacier
1. It is the movement of of rock particles by
wind, ice, and gravity.
2. The process that breaks down rocks and
other substances down.
3. It is an enormous mass of ice moving over the
land.
4. It is the breaking up of rocks when the water
in the cracks freezes and thaws.
5. It involves the breakdown of rocks and soils
through direct contact with atmospheric
conditions, such as heat, water, ice and
pressure.
Are you done class?
8. Agreement
Okay next meeting we are going to have
an activity about and soil erosion. I want
B. acid rain
A. tree roots can damage and break
down concrete
Erosion
Weathering
Glacier
Ice Wedging
Physical weathering
Yes, Teacher Knessa.
Goodbye and thank you Teacher
14. you to bring the following: rocks,
hammer, old newspaper, breaker and
vinegar
That’s all for today class.
Good bye.
Knessa.