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Wednesday, February 28, 2018
Saturday, February 24, 2018
Grade 3 Math and Science H.W
Feb.25- Mar.1
Date
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Math
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Science
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Sunday Feb.25
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Multiply by 5
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What are Fossils?
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Monday Feb.26
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Multiply by 5
HW: P.317-318
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What are Fossils?
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Tuesday Feb.27
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Divide by 5
HW: Sheet
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What are Fossils?
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Wednesday Feb.28
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Divide by 5
HW: P.323-324
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What are Fossils?
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Thursday Mar.1
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Problem solving
HW: Sheet
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HW: Answer the sheet
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Multiply by 5 | Learn Multiplication | Multiply By Music | Jack Hartmann
Saturday, Feb. 24 2018
Last week we started multiplication and this week we will go on
Multiplay by 5
Last week we started multiplication and this week we will go on
Multiplay by 5
Saturday Feb. 24,2018
This week we will study the different kinds of Fossils.
I will upload a video and the lesson from the book to help you understand the lesson.
Lesson 3: What Are Fossils?
Vocabulary
Fossils
Think about the “fossils” you made in the Investigate. Did they look like the shell you used? How were they different from the shell? A fossil is a trace or the remains of a living thing that died a long time ago. There are many different kinds of fossils.
Some fossils, such as bones and teeth, look like the actual parts of animals. Slowly minerals replaced the bones.
Other fossils, such as dinosaur tracks in mud, are only marks left behind. These marks are called imprints. The mud hardened, and in time it changed to rock. Some imprints are of animal parts, such as feathers. Other imprints are of leaves
A mold is the shape of a once-living thing left in sediment when
the rock formed. The organism that made the mold dissolved, leaving only a cavity
shaped like the organism.
A cast forms when mud or minerals later fill a mold. The cast has
the actual shape of the organism itself. You made a model of a fossil mold and
a fossil cast in the Investigate.
Plant fossils are not as common as animal fossils. That’s because
the soft parts of plants are easily destroyed as rocks form.
MAIN
IDEA AND DETAILS What are three
kinds of fossils?
This fossil shows a trilobite, a
kind of animal that died out more than 200 million years ago.
This fossil shows a trilobite, a
kind of animal that died out more than 200 million years ago.
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How Fossils Form
Places
that have a lot of sedimentary rocks are better for fossil hunting than other
places. Why? It’s because what’s left of a once-living thing is sometimes
buried in the particles that form sedimentary rock. Fossils often form in
limestone and shale.
Few
fossils form in metamorphic and igneous rock. The pressure and temperature that
form these rocks often destroy plant and animal parts before they can become
fossils.
The Science Up Close shows how a fossil might have begun forming
millions of years ago. After dying, the animal was quickly covered by layers of
sediment. If the animal had not been covered quickly, another animal might have
eaten it. After millions of years, the layers of sediment became sedimentary
rock. What was left of the animal is now a fossil.
MAIN
IDEA AND DETAILS Why are more
fossils found in sedimentary rocks than in other rocks?
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This
shows what the triceratops fossil below might look like
What can a scientist tell
about this fossil?
Learning from Fossils
Scientists
today use fossils to learn about animals and plants that no longer exist. For
example, scientists learn what kind of foods animals ate by looking at the
shapes of fossil teeth. The teeth are compared to those of today’s animals.
Fossils
also help scientists tell what a place was like long ago. For example, fossil
clams in a place show that a sea once covered the area.
Wednesday, February 21, 2018
Saturday, February 17, 2018
Grade 3 Math and Science H.W
Feb.18- Feb 22
Date
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Math
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Science
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Sunday Feb.18
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Patterns in the Multiplication
Table
No H.W
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What are types of rocks?
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Monday Feb.19
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Patterns in the Multiplication
Table
HW: Book p.299-300
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What are types of rocks?
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Tuesday Feb.20
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Multiply by 2
HW: Sheet
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What are types of rocks?
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Wednesday Feb.21
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Multiply by 2
HW: Book p. 305-306
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What are types of rocks?
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Thursday Feb.22
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Divide by 2
HW: Study table 2
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Due date for the project
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Tuesday, February 13, 2018
Saturday, February 10, 2018
Grade 3 Math and Science H.W
Feb.11- Feb 15
Date
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Math
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Science
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Sunday Feb.11
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Relate Division and Multiplication
H.W: Sheet
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What are types of rocks?
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Monday Feb.12
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Relate Division and Multiplication
H.W: Book p.269-270
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What are types of rocks?
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Tuesday Feb.13
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Inverse Operation
H.W: Sheet
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What are types of rocks?
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Wednesday Feb.14
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Inverse Operation
H.W: Book p.275-276
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What are types of rocks?
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Thursday Feb.15
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Math activities
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Answer in the practice book
H.W :Answer the sheet
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This week and next week we will study the different kinds of Rocks.
I will upload 2 videos and the lesson from the book to help you understand the lesson.
What Are the Types of Rocks?
VOCABULARY
Types of Rocks
Suppose you want to start a rock collection. How would you group the rocks? By color, by grain size, by whether they have layers? Rocks can look very different, but there are just three main types of rocks. The three types of rocks are grouped by how they form.
Igneous rock is a rock that was once melted and then cooled and hardened. Some igneous rocks cool quickly and look like glass. Other igneous rocks cool more slowly and have large grains.
Rock that forms from material that has settled into layers is
called Sedimentary rock. The layers are squeezed together until they form rock.
The third type of rock is called metamorphic rock. Metamorphic
rock is rock that has been changed by temperature and pressure.
How Rocks Form
The three types of rock
form differently. Melted rock can reach Earth’s surface through a volcano. Then
it cools and becomes igneous rock.
Sedimentary rock, by contrast, begins with the breaking of rocks.
Wind and water break rock into bits. Then the wind and water carry the bits of
rock and soil away. The bits settle into layers. After a long time, the layers
harden into rock.
Metamorphic rock forms deep in Earth’s crust in yet another way.
The pressure and temperature there change rock into metamorphic rock.
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Wind and water break rock into small bits. Then wind and water carry away the bits of rock. Layers of these bits of rock form and, under pressure, become sedimentary rock.
Wind and water break rock into small bits. Then wind and water carry away the bits of rock. Layers of these bits of rock form and, under pressure, become sedimentary rock.
Rock inside Earth softens from Earth’s high heat.Pressure in Earth’s crust then squeezes the rock. The rock changes into metamorphic rock.
The Rock Cycle
Over
time, one kind of rock can become any other kind. The process of rocks changing
from one kind of rock to another kind of rock is called the rock cycle. The
diagram on the right page shows this cycle.
Wind and
water break down all kinds of rocks to form sedimentary rocks. Any kind of rock
that melts and cools can become an igneous rock. Any rock can end up in Earth’s
crust and be pressed and heated. Then that rock can become metamorphic rock.
The Rock Cycle
Over
time, one kind of rock can become any other kind. The process of rocks changing
from one kind of rock to another kind of rock is called the rock cycle. The
diagram on the right page shows this cycle.
Wind and
water break down all kinds of rocks to form sedimentary rocks. Any kind of rock
that melts and cools can become an igneous rock. Any rock can end up in Earth’s
crust and be pressed and heated. Then that rock can become metamorphic rock.
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