changes to earth’s land
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Changes to Earth’s Land. Grade 3 SS3E2 Students will investigate fossils as evidence of organisms that lived long ago. What is weathering?. Weathering is the slow breaking apart or wearing away of rock into smaller pieces. - PowerPoint PPT PresentationTRANSCRIPT
Changes to Earth’s Land
Grade 3 SS3E2 Students will investigate fossils as evidence
of organisms that lived long ago
What is weathering?
Weathering is the slow breaking apart or wearing away of rock into smaller pieces.
Moving water, wind, ice and growing plants roots can all cause weathering.
How does weathering happen?• In Georgia, most weathering is caused by moving
water. Rocks rub against each other and become worn down. The rocks become smoother and smaller.
• Wind causes weathering when it picks up rock particles and blows them against larger rocks. This wears the rocks away.
• Changes in weather can also cause weathering. If water seeps into cracks of rocks and freezes , the cracks can get bigger.
• Plants are another cause of weathering. Plants can grow into the cracks, which causes the cracks to widen. Growing roots can break apart even large rocks.
Erosion• Once a rock is broken down by weathering, the
smaller pieces can be moved by water, winder or ice in an process called erosion.
• Erosion is the movement of weathered rock from one location to another.
• Georgia’s Providence Canyon was formed by Erosion
• http://www.gastateparks.org/ProvidenceCanyonrosion
• Ocean wave erosion can change shorelines. Waves can wash away sand and rock.
• Erosion can cause caves to form. • Ellison’s Cave is an example.
Other cause of erosion
• Wind is another cause of erosion. It can make loose bits of sand and soil roll and bounce across the land.
• Wind can cause particles and soil to rub against rocks. New rock shapes are carved by wind over time.
• Gravity causes erosion. This force pulls soil and rocks downhill. Gravity also moves glaciers. A glacier is a large mass of slow moving ice that flows down a slope. As a glacier moves, it collects rocks and soil. A glacier can carves out mountainsides to make valleys and canyons.
Deposition
• Erosion by water, wind, or ice moves particles of sand, soil and bits of rock called sediment.
• Over time, this sediment is dropped to a new place.• The dropping of sediment by wind, water, ice or
gravity is called deposition.• Deposition along the shore causes beaches to form.
This happens when ocean waves crash into land, depositing sand, rocks and shells.
• Rivers carry sediment downhill towards lakes and oceans. As the land flattens, sediment is dropped. If this process occurs at the mouth of the river, a large mass of deposited sediment, a delta is formed.
What’s in Soil?• Most plants need soil in order to grow. Soil is loose
material that covers most of the Earth’s surface. Soil is made up of bits of rock, minerals, and material that was once living.
• Soil is formed when rocks are weathered. After thousands of years, weather rocks mix with humus to become soil.
• Humus is the decayed remains of plants and animals.
Types of Soil• Sandy soil – particles are medium sized and
very hard.• Silt soil is soft, smooth soil that contains slightly
larger particles than clay• Clay soil is made up of very small, tightly-
packed particles.
Types of Soil• The particle size in the soil affects the way water
drains through soil.• Water passes through the large particles that
make up sandy soil. It passes less easily through smaller particles that make up silt soil.
• When clay particles get wet, they stick together. Water drains very slowly through clay soil.
• Many plants grown well in loam. • Loam is a mixture of sand, silt, clay and humus.
Soil Layers• When wind, moving water, and moving ice slow
down, they drop the sediment they are carrying. Over time, soil particles and larger pieces of rock build up and form layers of soil.
• There are three main layers.• The uppermost layer is topsoil. Plants grow best
in topsoil since it contains humus.• The layer below topsoil is called subsoil. Subsoil
contains little humus.• Bedrock is the solid rock that lies below subsoil.
Types of SoilSoil is made up of bits of rock, minerals, and material
from once living things. Soils are classified by the type of rock bits they contain. Clay soil has tiny particles packed tightly together. Topsoil and subsoil are soil
layers that lie above bedrock
Fossils• Fossils, the remains of once-living things, give
clues about living things long ago.• Scientists know what the Earth is like long ago by
studying rocks and fossils found in these rocks.• A fossil is the preserved remains of a plant or
animal that lived long ago.• Fossils include bones, teeth, shells, and imprints of
organisms that were pressed in mud and sand.• A scientist who studies fossils and organisms is
called a paleontologist.
How do fossils form?• Some fossils from when plants and animals die
and are buried in the soil.• Some fossils form when organisms die and
leave imprints in wet soil. Other imprints come from the footprints of organisms.
• Fossils are only part of once-living thing. That’s why studying one fossil does not always tell everything about an organism.
Kinds of Fossils• Fossils can form in many ways. Imprints, molds
and casts are three kinds of fossils.• Fossils can be organisms or their parts
preserved in different materials. Amber, hardened mud, rock, tar, and ice are materials in which fossils have been found.
Fossils• Some fossils are called “petrified”
fossils. A common example is petrified wood. This happens when a fossil forms on a tree once it has died.
Record in the Rocks• Earth’s surface has changed over millions of
years. • Fossils can give clues about some changes
that have taken place.• Fossils of plants and animals that lived in
warm regions have been found in places that are now very cold. This shows that the weather in some places on Earth has changed over time.
Georgia’s State Fossil• Georgia’s state fossil is the shark’s tooth.
• Summary• A fossil is the preserved remains of a plant or
animal that lived long ago.• Fossils include imprints, molds, casts, and
preserved remains in amber.• Fossils can give us clues about what Earth’s
surface was once like and how it has changed.
A imprint of an animal that lived long ago is not likely to
give clues about that animal’sA. ShapeB. ColorC. SizeD. weight