Rocks are made of minerals and vary in durability, shape, color, and texture, while minerals are nonliving solids formed in nature that are more lustrous and durable than rocks. Both are classified by their physical properties and hardness can be determined by chipping, streaking, and scratching. Soil types like clay, sand, and loam differ in their composition, drainage, and ability to support plant growth. Fossils form when remains of once-living organisms become preserved in rock layers over time. Georgia contains diverse habitats for different plants and animals, including mountains, marshes, coasts, and forests. Heat is a form of energy transferred by temperature difference through radiation, conduction, or convection
The author conducted field research at three locations, observing rocks, trees, plants, and animals. At the third location, a hike near Heavenly, the author found most of the samples and learned more about their surroundings. Samples included mafic diorite and brown chert rocks, Jeffrey pine trees containing ant nests, Collomia linearis and Penstemon newberryi plants, and tree borers on a fallen log. The author documented principles of geology observed like weathering, erosion, inclusions and unconformities.
Rocks are non-living parts of the Earth that come in various sizes, shapes, and colors. For thousands of years, rocks have been used for tools, statues, and other purposes. Rocks can be found underground, under bodies of water, and on land. Different types of rocks like slate, granite, chalk, and marble are used to make roof tiles, kitchen tables, chalk, and statues, respectively. Rocks are composed of minerals, with some minerals like graphite, magnetite, and fluorite having applications in pencils, magnets, and toothpaste.
This document provides an overview of Earth's history and geology. It explains that Earth is geologically active with huge amounts of energy acting on its surface and interior. Observable evidence today can provide information about past processes and events. It then describes various aspects of Earth's structure like the crust, mantle, core and tectonic plates. It discusses geological processes like erosion, sedimentation, and the rock cycle. It also outlines plate tectonics and features at plate boundaries like divergent, convergent and transform boundaries. Key terms are defined like seismic, fossil, and stratigraphy. The conclusion notes that rather than being serene, Earth is a dynamic world that is constantly changing.
1. Rocks are made up of minerals and can be found deep underground in mines or near the surface in quarries.
2. Minerals have unique properties like hardness, lustre, and color that allow them to be identified. They are used to make construction materials, obtain metals, and create jewelry.
3. Soil is formed over long periods of time as rocks are broken down by weathering and mixed with decaying matter. It is made up of layers with different materials and must be protected to support plant growth.
This document discusses minerals, rocks, and soil. It explains that minerals are non-living, solid materials found in the earth that have properties like luster, color, and hardness. It describes how different types of rocks like igneous, sedimentary, and metamorphic rocks form. It also explains that soil is formed from weathered rocks and decaying organisms and provides nutrients for plants and animals.
Minerals form by natural geological processes and have distinct physical properties that allow them to be identified and classified. They are solid, naturally occurring inorganic substances with a definite chemical composition and crystalline structure (atoms arranged in repeating patterns). Key properties used to identify minerals include their color, hardness, luster, density/specific gravity, streak, breakage patterns, and unique characteristics. Minerals have many important uses from jewelry to industrial applications.
Rocks form the Earth's outer layer and are composed of minerals. There are three main types of rocks: igneous rocks which form from cooling magma, sedimentary rocks which form from compressed sediments, and metamorphic rocks which form from changes to existing igneous and sedimentary rocks. Igneous rocks such as granite are used in construction while sedimentary rocks such as limestone can be used as a building material. The mining industry extracts various rocks and minerals for use in construction and other applications but can also negatively impact the environment.
The document discusses minerals and rocks. It defines minerals as solid, natural materials made from nonliving substances in the ground and made up of elements. It describes properties of minerals such as luster, hardness, cleavage, and fracture. It also discusses the shapes of minerals including crystals and gems. The document then defines rocks and describes the three main types: sedimentary rocks form from compressed sediments, igneous rocks form when lava cools and hardens, and metamorphic rocks form from changes to sedimentary and igneous rocks under heat and pressure.
The author conducted field research at three locations, observing rocks, trees, plants, and animals. At the third location, a hike near Heavenly, the author found most of the samples and learned more about their surroundings. Samples included mafic diorite and brown chert rocks, Jeffrey pine trees containing ant nests, Collomia linearis and Penstemon newberryi plants, and tree borers on a fallen log. The author documented principles of geology observed like weathering, erosion, inclusions and unconformities.
Rocks are non-living parts of the Earth that come in various sizes, shapes, and colors. For thousands of years, rocks have been used for tools, statues, and other purposes. Rocks can be found underground, under bodies of water, and on land. Different types of rocks like slate, granite, chalk, and marble are used to make roof tiles, kitchen tables, chalk, and statues, respectively. Rocks are composed of minerals, with some minerals like graphite, magnetite, and fluorite having applications in pencils, magnets, and toothpaste.
This document provides an overview of Earth's history and geology. It explains that Earth is geologically active with huge amounts of energy acting on its surface and interior. Observable evidence today can provide information about past processes and events. It then describes various aspects of Earth's structure like the crust, mantle, core and tectonic plates. It discusses geological processes like erosion, sedimentation, and the rock cycle. It also outlines plate tectonics and features at plate boundaries like divergent, convergent and transform boundaries. Key terms are defined like seismic, fossil, and stratigraphy. The conclusion notes that rather than being serene, Earth is a dynamic world that is constantly changing.
1. Rocks are made up of minerals and can be found deep underground in mines or near the surface in quarries.
2. Minerals have unique properties like hardness, lustre, and color that allow them to be identified. They are used to make construction materials, obtain metals, and create jewelry.
3. Soil is formed over long periods of time as rocks are broken down by weathering and mixed with decaying matter. It is made up of layers with different materials and must be protected to support plant growth.
This document discusses minerals, rocks, and soil. It explains that minerals are non-living, solid materials found in the earth that have properties like luster, color, and hardness. It describes how different types of rocks like igneous, sedimentary, and metamorphic rocks form. It also explains that soil is formed from weathered rocks and decaying organisms and provides nutrients for plants and animals.
Minerals form by natural geological processes and have distinct physical properties that allow them to be identified and classified. They are solid, naturally occurring inorganic substances with a definite chemical composition and crystalline structure (atoms arranged in repeating patterns). Key properties used to identify minerals include their color, hardness, luster, density/specific gravity, streak, breakage patterns, and unique characteristics. Minerals have many important uses from jewelry to industrial applications.
Rocks form the Earth's outer layer and are composed of minerals. There are three main types of rocks: igneous rocks which form from cooling magma, sedimentary rocks which form from compressed sediments, and metamorphic rocks which form from changes to existing igneous and sedimentary rocks. Igneous rocks such as granite are used in construction while sedimentary rocks such as limestone can be used as a building material. The mining industry extracts various rocks and minerals for use in construction and other applications but can also negatively impact the environment.
The document discusses minerals and rocks. It defines minerals as solid, natural materials made from nonliving substances in the ground and made up of elements. It describes properties of minerals such as luster, hardness, cleavage, and fracture. It also discusses the shapes of minerals including crystals and gems. The document then defines rocks and describes the three main types: sedimentary rocks form from compressed sediments, igneous rocks form when lava cools and hardens, and metamorphic rocks form from changes to sedimentary and igneous rocks under heat and pressure.
The document discusses the rock cycle and how rocks are formed and transformed. It describes the three main rock types - igneous, sedimentary, and metamorphic - and the processes involved in their formation. Igneous rocks form from the cooling of magma, either deep underground or at the surface. Sedimentary rocks form from the compaction and cementation of sediments. Metamorphic rocks form from changes to existing rocks via heat, pressure, and chemical reactions in the Earth. The rock cycle diagram shows how rocks continuously transform between these three types through geological processes over long periods of time.
There are three main types of rocks:
1) Igneous rocks form from solidified magma either below or above the surface.
2) Sedimentary rocks form from compressed and cemented sediment.
3) Metamorphic rocks form from existing igneous or sedimentary rocks that have been altered by heat and pressure.
The document defines geology as the study of the Earth and its forces and processes. It explains the principle of uniformitarianism, which states that geologic processes operating today also operated in the past. This allows geologists to understand Earth's history. The document describes the three main types of rocks - igneous, sedimentary, and metamorphic - and explains the rock cycle by which rocks are constantly being formed and transformed through geological processes like erosion, deposition, melting, and crystallization.
Metals are strong, hard, and difficult to break. They are very good conductors of heat and electricity. Most metals are dense, silvery in color, and have high melting and boiling points. Metals are solids at room temperature, except for mercury which is liquid, and can be shaped through hammering while malleable or stretching thinly while ductile.
This document provides an overview of minerals, rocks, and energy resources related to the lithosphere and hydrosphere. It defines minerals as naturally occurring inorganic substances with distinct compositions and structures. It describes how minerals are classified based on properties like color, transparency, hardness, and streak. It also discusses the formation and classification of different rock types. Finally, it examines various energy resources derived from the lithosphere and hydrosphere, including fossil fuels, uranium, geothermal, hydropower, and renewable sources.
The document discusses the interior structure of the Earth. It is composed of several concentric layers, with the crust being the outermost layer. Below the crust is the mantle, which extends to a depth of 2,900 km. The innermost layer is the core, with a radius of around 3,500 km. The Earth's crust is made up of various rock types, including igneous, sedimentary, and metamorphic rocks. Rocks undergo changes in a cyclic process called the rock cycle, where they can transform from one type to another over time through processes like cooling of magma, weathering and erosion, deposition, and changes in pressure and temperature.
The document contains information about different types of rocks presented across 12 cards. It discusses the classification of rocks by their textures, how they are formed from minerals and sediments, and key characteristics. Igneous rocks such as granite form from cooling magma and volcanism. Sedimentary rocks like limestone and sandstone form through compaction and cementation of sediments. Metamorphic rocks change form due to heat and pressure acting on existing rocks.
1) There are three major types of rock: igneous, sedimentary, and metamorphic.
2) All new rock starts as igneous rock, formed from cooled lava or magma.
3) Igneous rock can be intrusive or extrusive depending on whether the magma cools below or above the surface.
The document discusses the three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from solidified magma or lava. Sedimentary rocks form from compression of sediments or remains of living things. Metamorphic rocks form from changes to pre-existing rocks through heat, pressure, and chemical reactions. Each rock type has distinct characteristics and modes of formation.
Minerals are naturally occurring inorganic substances that make up rocks. Rocks can be classified as igneous, sedimentary, or metamorphic based on how they are formed. Igneous rocks form from the cooling of magma either below or above the Earth's surface. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form when existing rocks are subjected to heat and pressure, causing them to recrystallize without melting. Minerals can be identified based on properties like color, streak, luster, hardness, fracture, crystal form, specific gravity, and others.
The document discusses different types of rocks:
1. Igneous rocks form from cooling magma and include intrusive granitic rocks, extrusive volcanic rocks like basalt, and hypabyssal rocks.
2. Sedimentary rocks form through the lithification of sediments and include clastic rocks like sandstone, chemical rocks like limestone, and organic rocks like coal.
3. Metamorphic rocks form from the alteration of existing rocks under heat, pressure, and fluids, changing their texture and minerals. Foliated rocks include schist and gneiss, while non-foliated rocks include marble and quartzite.
- Formation and evolution of soil.
- Characteristics and classification of soils.
- Regularity and environmental features of soil distribution on Earth.
- Location of the soil in the biosphere.
- Morphological signs of soil profile.
- Structure of soil profile.
- Granulometric composition.
- Soil composition: properties and modes.
- General physical properties of soil.
1. The document discusses two external forces that change the Earth's surface: weathering and erosion. Weathering is the breakdown of rocks in place through mechanical or chemical processes, while erosion is the transport of weathered materials by agents such as water, wind, and waves.
2. Mechanical weathering includes exfoliation through thermal expansion and contraction, frost shattering through freezing water in cracks, and the widening of cracks by plant and animal roots. Chemical weathering occurs through solution in carbonic acid or oxidation that breaks down iron in rocks.
3. Erosion shapes landforms as water, wind, and waves carry sediments that abrade rock surfaces, enlarging cracks to form features such as
The rock cycle shows how the three main rock types - igneous, sedimentary, and metamorphic - are interrelated and constantly transforming into one another over geological time through various natural processes. Igneous rocks form from the cooling of magma, sedimentary rocks form through the lithification of sediments, and metamorphic rocks form under high heat and pressure which causes changes to pre-existing rocks. Rocks are constantly being recycled and transformed as they move through the rock cycle.
The document discusses the layers that make up the interior of the Earth. It describes three major layers - the crust, mantle, and core. The crust is the outermost solid rocky layer that makes up the continents and ocean floors. Below the crust is the mantle, which extends almost 3000 km deep. The innermost layer is the core, composed primarily of iron and nickel. The core is over 3500 km in radius and responsible for the Earth's magnetic field. Rocks on the surface are continuously changing between igneous, sedimentary, and metamorphic types in the rock cycle.
Fossils provide evidence about past life on Earth. A fossil forms when an organism is buried after death and the remains are slowly replaced with minerals over millions of years. Fossils give clues about ancient environments and organisms, and help show how life has evolved over time. The fossil record is incomplete as only a small fraction of organisms become fossilized.
Fossils provide evidence about past life on Earth. A fossil forms when an organism is buried after death and the remains are slowly replaced with minerals over millions of years. Fossils give clues about ancient environments and organisms, and help show how life has evolved over time. The fossil record is incomplete as only a small fraction of organisms become fossilized.
Rocks are naturally occurring mixtures that can be divided into three main types - igneous, sedimentary, and metamorphic - based on their formation process. Igneous rocks form from cooling magma or lava. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from changes to existing rocks through heat, pressure, and other processes in the Earth. Rocks continually change between these types through the rock cycle as they are weathered, eroded, melted, cooled, and compacted over time.
Minerals and rocks are naturally occurring inorganic solids with distinct chemical compositions and physical properties. There are over 3,000 known minerals that make up rocks. Minerals are studied in mineralogy and have properties like color, streak, hardness, cleavage, and density that are used to identify them. Rocks form from the accumulation of minerals and other materials through natural processes. There are three main types of rocks: igneous rocks that form from cooled magma, sedimentary rocks that form from compressed sediments, and metamorphic rocks that form from existing rocks undergoing changes due to heat and pressure in Earth's crust.
The document discusses the rock cycle and how rocks are formed and transformed. It describes the three main rock types - igneous, sedimentary, and metamorphic - and the processes involved in their formation. Igneous rocks form from the cooling of magma, either deep underground or at the surface. Sedimentary rocks form from the compaction and cementation of sediments. Metamorphic rocks form from changes to existing rocks via heat, pressure, and chemical reactions in the Earth. The rock cycle diagram shows how rocks continuously transform between these three types through geological processes over long periods of time.
There are three main types of rocks:
1) Igneous rocks form from solidified magma either below or above the surface.
2) Sedimentary rocks form from compressed and cemented sediment.
3) Metamorphic rocks form from existing igneous or sedimentary rocks that have been altered by heat and pressure.
The document defines geology as the study of the Earth and its forces and processes. It explains the principle of uniformitarianism, which states that geologic processes operating today also operated in the past. This allows geologists to understand Earth's history. The document describes the three main types of rocks - igneous, sedimentary, and metamorphic - and explains the rock cycle by which rocks are constantly being formed and transformed through geological processes like erosion, deposition, melting, and crystallization.
Metals are strong, hard, and difficult to break. They are very good conductors of heat and electricity. Most metals are dense, silvery in color, and have high melting and boiling points. Metals are solids at room temperature, except for mercury which is liquid, and can be shaped through hammering while malleable or stretching thinly while ductile.
This document provides an overview of minerals, rocks, and energy resources related to the lithosphere and hydrosphere. It defines minerals as naturally occurring inorganic substances with distinct compositions and structures. It describes how minerals are classified based on properties like color, transparency, hardness, and streak. It also discusses the formation and classification of different rock types. Finally, it examines various energy resources derived from the lithosphere and hydrosphere, including fossil fuels, uranium, geothermal, hydropower, and renewable sources.
The document discusses the interior structure of the Earth. It is composed of several concentric layers, with the crust being the outermost layer. Below the crust is the mantle, which extends to a depth of 2,900 km. The innermost layer is the core, with a radius of around 3,500 km. The Earth's crust is made up of various rock types, including igneous, sedimentary, and metamorphic rocks. Rocks undergo changes in a cyclic process called the rock cycle, where they can transform from one type to another over time through processes like cooling of magma, weathering and erosion, deposition, and changes in pressure and temperature.
The document contains information about different types of rocks presented across 12 cards. It discusses the classification of rocks by their textures, how they are formed from minerals and sediments, and key characteristics. Igneous rocks such as granite form from cooling magma and volcanism. Sedimentary rocks like limestone and sandstone form through compaction and cementation of sediments. Metamorphic rocks change form due to heat and pressure acting on existing rocks.
1) There are three major types of rock: igneous, sedimentary, and metamorphic.
2) All new rock starts as igneous rock, formed from cooled lava or magma.
3) Igneous rock can be intrusive or extrusive depending on whether the magma cools below or above the surface.
The document discusses the three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from solidified magma or lava. Sedimentary rocks form from compression of sediments or remains of living things. Metamorphic rocks form from changes to pre-existing rocks through heat, pressure, and chemical reactions. Each rock type has distinct characteristics and modes of formation.
Minerals are naturally occurring inorganic substances that make up rocks. Rocks can be classified as igneous, sedimentary, or metamorphic based on how they are formed. Igneous rocks form from the cooling of magma either below or above the Earth's surface. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form when existing rocks are subjected to heat and pressure, causing them to recrystallize without melting. Minerals can be identified based on properties like color, streak, luster, hardness, fracture, crystal form, specific gravity, and others.
The document discusses different types of rocks:
1. Igneous rocks form from cooling magma and include intrusive granitic rocks, extrusive volcanic rocks like basalt, and hypabyssal rocks.
2. Sedimentary rocks form through the lithification of sediments and include clastic rocks like sandstone, chemical rocks like limestone, and organic rocks like coal.
3. Metamorphic rocks form from the alteration of existing rocks under heat, pressure, and fluids, changing their texture and minerals. Foliated rocks include schist and gneiss, while non-foliated rocks include marble and quartzite.
- Formation and evolution of soil.
- Characteristics and classification of soils.
- Regularity and environmental features of soil distribution on Earth.
- Location of the soil in the biosphere.
- Morphological signs of soil profile.
- Structure of soil profile.
- Granulometric composition.
- Soil composition: properties and modes.
- General physical properties of soil.
1. The document discusses two external forces that change the Earth's surface: weathering and erosion. Weathering is the breakdown of rocks in place through mechanical or chemical processes, while erosion is the transport of weathered materials by agents such as water, wind, and waves.
2. Mechanical weathering includes exfoliation through thermal expansion and contraction, frost shattering through freezing water in cracks, and the widening of cracks by plant and animal roots. Chemical weathering occurs through solution in carbonic acid or oxidation that breaks down iron in rocks.
3. Erosion shapes landforms as water, wind, and waves carry sediments that abrade rock surfaces, enlarging cracks to form features such as
The rock cycle shows how the three main rock types - igneous, sedimentary, and metamorphic - are interrelated and constantly transforming into one another over geological time through various natural processes. Igneous rocks form from the cooling of magma, sedimentary rocks form through the lithification of sediments, and metamorphic rocks form under high heat and pressure which causes changes to pre-existing rocks. Rocks are constantly being recycled and transformed as they move through the rock cycle.
The document discusses the layers that make up the interior of the Earth. It describes three major layers - the crust, mantle, and core. The crust is the outermost solid rocky layer that makes up the continents and ocean floors. Below the crust is the mantle, which extends almost 3000 km deep. The innermost layer is the core, composed primarily of iron and nickel. The core is over 3500 km in radius and responsible for the Earth's magnetic field. Rocks on the surface are continuously changing between igneous, sedimentary, and metamorphic types in the rock cycle.
Fossils provide evidence about past life on Earth. A fossil forms when an organism is buried after death and the remains are slowly replaced with minerals over millions of years. Fossils give clues about ancient environments and organisms, and help show how life has evolved over time. The fossil record is incomplete as only a small fraction of organisms become fossilized.
Fossils provide evidence about past life on Earth. A fossil forms when an organism is buried after death and the remains are slowly replaced with minerals over millions of years. Fossils give clues about ancient environments and organisms, and help show how life has evolved over time. The fossil record is incomplete as only a small fraction of organisms become fossilized.
Rocks are naturally occurring mixtures that can be divided into three main types - igneous, sedimentary, and metamorphic - based on their formation process. Igneous rocks form from cooling magma or lava. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from changes to existing rocks through heat, pressure, and other processes in the Earth. Rocks continually change between these types through the rock cycle as they are weathered, eroded, melted, cooled, and compacted over time.
Minerals and rocks are naturally occurring inorganic solids with distinct chemical compositions and physical properties. There are over 3,000 known minerals that make up rocks. Minerals are studied in mineralogy and have properties like color, streak, hardness, cleavage, and density that are used to identify them. Rocks form from the accumulation of minerals and other materials through natural processes. There are three main types of rocks: igneous rocks that form from cooled magma, sedimentary rocks that form from compressed sediments, and metamorphic rocks that form from existing rocks undergoing changes due to heat and pressure in Earth's crust.
1. Rocks and Minerals
Rocks VS. Minerals
•Made of minerals (nonliving • nonliving solid formed in
solid formed in nature) nature
•Vary with durability •More luster than rocks
•Classified by shape, color, and •Are durable
texture
•Classified by shape, color,
•Determine hardness by and texture
chipping, streaking, and
•Determine hardness by
scratching
chipping, streaking, and
scratching
Clay Sand Loam
• type of topsoil that has small • Sand contains loose particles of • same as potting soil
grains weathered rocks with little humus
•Best soil for growing plants
material.
•holds water easily
•Large particles
•Color is shades of red, •Water drains through easily
orange and brown •Doesn’t support plant life
•Plants do not grow well in
clay
Extra Facts:
Topsoil made from weathered rocks, humus, air, and water.
Topsoil is a loose material in which plants can grow.
Erosion is the movement of weathered rock and soil.
Wind, water, and ice erode rocks through the process of weathering to form soils.
Erosion and weathering change the appearance and integrity of rocks and soils over time.
2. Fossils
fossil is something that has lasted
from a living thing that died
long ago
mold is the shape of a plant or cast mold
animal left in sediments
when the rock formed
imprint are molds of leaves or other imprint
thin objects (an imprint is a
lot like a stamp)
cast forms when mud or minerals cast mold
fill a mold and hardens
A fossil is the remains formed from a living thing (plant or animal) that died long ago.
Mold, cast, and imprint are types of fossils.
Fossils are formed when a living thing’s remains (bone/shell/stem/leaves) are covered with
material from layers by nature.
3. Georgia Habitats
• A habitat is a place where both
plants and animals live.
• Mountains are landforms that are
much higher than the areas
around it.
• Marsh/swamp is a low lying
wetland with grass plants.
• Coastal land is located near a
large body of water such as a sea
or an ocean, and is known for its
climate.
• Atlantic Ocean is the body of salt
water that contains marine
animals.
• Piedmont is land between the
coastal plain and Appalachian
Mountains.
• Different organisms/plants live in
different habitats.
• Organisms/plants may not survive
if their habitat is changed.
4. Heat
Thermal energy (heat) • Heat is a form of energy
is produced by: that is transferred by a
difference in temperature.
Burning sun oven
• Friction is the force
friction between two moving
objects that prevents them
from moving freely.
• Insulation is material that
heat cannot move through
easily.
• Radiation is heat energy
Insulators vs. conductors that is passed without
touching anything.
• Heat is transferable
through different objects.
• A thermometer is a tool
used to measure
temperature.
5. Magnets
• Magnets are usually Some things magnets are attracted to
metallic objects that (stick to): metals
attract each other and
some other objects.
• Some objects are
attracted by magnets
while some are not.
• Magnets have two parts:
a north pole and a south Some things magnets are NOT
pole. attracted to:
• The north pole of one
magnet attracts the south
pole of another magnet
(opposites attract).
• Similar poles of two
magnets repel each other Opposite poles attract (come together):
(alike repels).
Like poles repel (push apart):
6. Pollution
Types of Pollution: Some Facts
• Pollution occurs when the environment is contaminated
Air: with harmful substances.
• Human behaviors such as littering, driving, industry, and
development impact the environment. It effects plants and
animals.
• Conservation of resources and recycling of materials and
Water: reusing materials are ways to protect the environment.
.
Things you can do to reduce:
Say no to junk mail! Buy in bulk. Start a compost pile. Buy only what
Land: you need, instead of what you want.
Things you can reuse:
Clothes, travel cups, shopping bags, washable eating utensils
You can also donate items instead of throwing them away!
Noise:
Things you can recycle:
Acid Batteries, Aluminum Cans , Building Materials, Cardboard,
Chemicals, Electronic equipment, Glass (particularly bottles and jars),
Lead, Magazines, Metal, Newspaper, Oil, Paint, Paper, Plastic Bags,
Plastic Bottles, Steel Cans, Tires, White Goods (Appliances), Wood,
Writing/Copy Paper, Yard Waste
7. Pollution
Types of Pollution: Some Facts
• Pollution occurs when the environment is contaminated
Air: with harmful substances.
• Human behaviors such as littering, driving, industry, and
development impact the environment. It effects plants and
animals.
• Conservation of resources and recycling of materials and
Water: reusing materials are ways to protect the environment.
.
Things you can do to reduce:
Say no to junk mail! Buy in bulk. Start a compost pile. Buy only what
Land: you need, instead of what you want.
Things you can reuse:
Clothes, travel cups, shopping bags, washable eating utensils
You can also donate items instead of throwing them away!
Noise:
Things you can recycle:
Acid Batteries, Aluminum Cans , Building Materials, Cardboard,
Chemicals, Electronic equipment, Glass (particularly bottles and jars),
Lead, Magazines, Metal, Newspaper, Oil, Paint, Paper, Plastic Bags,
Plastic Bottles, Steel Cans, Tires, White Goods (Appliances), Wood,
Writing/Copy Paper, Yard Waste