Examples of physical properties are: color, smell,
freezing point, boiling point, melting point, infra-red spectrum,
attraction (paramagnetic) or repulsion (diamagnetic) to magnets,
opacity, viscosity and density. There are many more examples.
Note that measuring each of these properties will not alter the
basic nature of the substance.
Examples of chemical properties are: heat of combustion,
reactivity with water, PH, and electromotive force.
The more properties we can identify for a substance, the better
we know the nature of that substance. These properties can then
help us model the substance and thus understand how this substance
will behave under various conditions.
Wednesday, December 31, 2014
Monday, December 15, 2014
Happy Holidays!
Happy Holidays!
Dear Parents,
Thank you for the support, kinds words, and gifts this past semester. Your thoughtfulness and generosity is deeply appreciated.
Mr. Shadow
Tuesday, December 2, 2014
Matter and 2nd Quarter Exam Study Guide
physical properties:Anything you can observe about an object by using your senses. Matter is classified by properties: state of matter, appearance, color, shape, size, texture, magnetic/nonmagnetic, conductor/insulator, odor, solubility...
solid:A form of matter that takes up a specific amount of space and has a definite shape. Its molecules are tightly packed together.
liquid:A form of matter that has a definite volume but no definite shape. Molecules are more loosely packed and move more freely.
gas:A form of matter that does not have a definite shape or a definite volume. Molecules move most freely.
melting process:Occurs when heat energy is applied and energy increases. When heat is applied, a solid turns to a liquid.
evaporation process:Occurs when more heat is applied; again energy increases and therefore, molecules move more rapidly. When heat is applied, a liquid turns to a gas.
condensation process:Occurs when molecules are cooled, condense and energy is lost. When cooled, a gas turns to a liquid. Clouds, dew, water droplets on the outside of a glass on a hot day are caused by condensation.
freezing process:Occurs when molecules are cooled even more, and more energy is lost. When cooled even more, a liquid turns to a solid.
plasma:A form of matter that, like gas, has no definite shape nor definite volume. Common forms of plasma include stars and neon signs.
mass:The measure of how much matter is contained in an object.
weight:The measure of the force (pull) of gravity between the Earth and an object.
density:A measure of how tightly packed matter is. The more matter that gets packed into the same amount of space, the more dense it is.
volume:The amount of space matter takes up.
boiling point:Refers to the temperature at which it boils; every substance has its own constant boiling point. Waters boiling point is 100C/212F.
melting point:Refers to the temperature at which it melts; every substance has its own constant melting point. Waters (ice) melting point is 0C/32F.
freezing point:Refers to the temperature at which it freezes; every substance has its own constant boiling point. Waters freezing point is 0C/32F.
grams or kilograms
Mass is measured in these metric units.
celsius
Metric unit for measuring temperature; on
this scale water freezes at zero and boils at 100. A Swedish astronomer
devised the centigrade thermometer, (1701-1744).
fahrenheit
A scale and unit of measurement for
temperature. It has been replaced in most countries by the Celsius
scale. A German physicist invented the mercury thermometer and developed
the scale of temperature that bears his name, (1686-1736).
scale
A tool used to measure weight.
graduated cylinder
A tool used to measure volume and density.
temperature
The measure of the amount of heat energy in the atmosphere.
physical state
The forms matter can be found in; examples are solid, liquid, and gas.
substance
Matter that has a uniform and unchanging composition.
balance scale
The balance scale is a tool used to measure the amount of mass in an object.
Wednesday, November 19, 2014
Tour of CERI, Chapter 4 Test, and WHY Project II
Tuesday, November 25th the 5th grade classes will walk to CERI to expand our knowledge of earthquakes.The continuing goal of CERI is to provide both scientific and non-scientific information
about earthquakes and earthquake preparedness to people in the central and eastern
U.S. who could someday be affected by a significant earthquake.
During the Iben Browning episode of 1990, CERI was the main regional source of earthquake
information. Filling the information vacuum during the period of intense public concern
had a permanent impact on public awareness and understanding of regional earthquake
hazards.
Why Project II forms will be sent home November 20th.
Due Date: December
15, 2014
All students are in the final phase
of the written component of their science research projects. They may now choose how to share their
research information. Examples are: poster, PowerPoint, Prezi, video,
demonstration, diorama, model, etc.
The project due date is Monday,
December 15th, 2014. I will check your progress Monday, December 8th. I will allow three homefun free weeks to
complete the presentation part of your WHYII project.
Friday, November 14, 2014
Earthquakes
Earthquakes can happen along any type
of plate boundary. They also occur along faults which are large cracks
in the earth’s crust. Most faults are associated with large plate
boundaries where violent earthquakes usually occur.
Causes of Earthquakes
An earthquake starts deep below the earth’s surface at the focus.
The focus is the point inside the Earth's crust where the pressure is released.
The epicentre of an earthquake is the position on the earth’s surface directly above its focus.
The jerking movement caused by plates sticking then moving releases built-up pressure inside the Earth's crust, in the form of seismic waves. The waves spread out from the focus.
The strongest waves are found near the centre of the earthquake. This
means that the most severe damage caused by an earthquake will happen
close to the epicentre.
It is almost impossible to predict when they will occur. The effect
of an earthquake depends on the depth of an earthquake as well as its magnitude.
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Thursday, November 6, 2014
Geological Features-Volcano/Earthquakes
What is a volcano?
A volcano is a mountain that opens downward to a pool of molten rock below the surface of the earth. When pressure builds up, eruptions occur. Gases and rock shoot up through the opening and spill over or fill the air with lava fragments. Eruptions can cause lateral blasts, lava flows, hot ash flows, mudslides, avalanches, falling ash and floods. Volcano eruptions have been known to knock down entire forests. An erupting volcano can trigger tsunamis, flash floods, earthquakes, mudflows and rockfalls.
Click Here to learn more about volcanoes from USGS.
How are volcanoes formed?
Volcanoes are formed when magma from within the Earth's upper mantle works its way to the surface. At the surface, it erupts to form lava flows and ash deposits. Over time as the volcano continues to erupt, it will get bigger and bigger.
What are the different stages of volcanoes?
Scientists have categorized volcanoes into three main categories: active, dormant, and extinct. An active volcano is one which has recently erupted and there is a possibility that it may erupt soon. A dormant volcano is one which has not erupted in a long time but there is a possibility it can erupt in the future. An extinct volcano is one which has erupted thousands of years ago and there’s no possibility of eruption.
Why do volcanoes erupt?
The Earth's crust is made up of huge slabs called plates, which fit together like a jigsaw puzzle. These plates sometimes move. The friction causes earthquakes and volcanic eruptions near the edges of the plates. The theory that explains this process is called plate tectonics.
What are plate tectonics?
The theory of plate tectonics is a interesting story of continents drifting from place to place breaking apart, colliding, and grinding against each other. The plate tectonic theory is supported by a wide range of evidence that considers the earth's crust and upper mantle to be composed of several large, thin, relatively rigid plates that move relative to one another. The plates are all moving in different directions and at different speeds. Sometimes the plates crash together, pull apart or sideswipe each other. When this happens, it commonly results in earthquakes.
Click Here to learn more about plate tectonics and the drifting of our continents.
How many volcanoes are there?
There are more than 1500 active volcanoes on the Earth. We currently know of 80 or more which are under the oceans. Active volcanoes in the U.S. are found mainly in Hawaii, Alaska, California, Oregon and Washington.
What are the different types of volcanoes?
Volcanoes are grouped into four types: cinder cones, composite volcanoes, shield volcanoes and lava volcanoes.
What is the difference between lava and magma?
Magma is liquid rock inside a volcano. Lava is liquid rock (magma) that flows out of a volcano. Fresh lava glows red hot to white hot as it flows.
A volcano is a mountain that opens downward to a pool of molten rock below the surface of the earth. When pressure builds up, eruptions occur. Gases and rock shoot up through the opening and spill over or fill the air with lava fragments. Eruptions can cause lateral blasts, lava flows, hot ash flows, mudslides, avalanches, falling ash and floods. Volcano eruptions have been known to knock down entire forests. An erupting volcano can trigger tsunamis, flash floods, earthquakes, mudflows and rockfalls.
Click Here to learn more about volcanoes from USGS.
How are volcanoes formed?
Volcanoes are formed when magma from within the Earth's upper mantle works its way to the surface. At the surface, it erupts to form lava flows and ash deposits. Over time as the volcano continues to erupt, it will get bigger and bigger.
What are the different stages of volcanoes?
Scientists have categorized volcanoes into three main categories: active, dormant, and extinct. An active volcano is one which has recently erupted and there is a possibility that it may erupt soon. A dormant volcano is one which has not erupted in a long time but there is a possibility it can erupt in the future. An extinct volcano is one which has erupted thousands of years ago and there’s no possibility of eruption.
Why do volcanoes erupt?
The Earth's crust is made up of huge slabs called plates, which fit together like a jigsaw puzzle. These plates sometimes move. The friction causes earthquakes and volcanic eruptions near the edges of the plates. The theory that explains this process is called plate tectonics.
What are plate tectonics?
The theory of plate tectonics is a interesting story of continents drifting from place to place breaking apart, colliding, and grinding against each other. The plate tectonic theory is supported by a wide range of evidence that considers the earth's crust and upper mantle to be composed of several large, thin, relatively rigid plates that move relative to one another. The plates are all moving in different directions and at different speeds. Sometimes the plates crash together, pull apart or sideswipe each other. When this happens, it commonly results in earthquakes.
Continental Drift: To see this animation again, just refresh this page! This animation shows you what our planet looked like millions of years ago and what it looks like now! (Graphic Credit: Geology Department at University of California, Berkeley) |
Click Here to learn more about plate tectonics and the drifting of our continents.
How many volcanoes are there?
There are more than 1500 active volcanoes on the Earth. We currently know of 80 or more which are under the oceans. Active volcanoes in the U.S. are found mainly in Hawaii, Alaska, California, Oregon and Washington.
What are the different types of volcanoes?
Volcanoes are grouped into four types: cinder cones, composite volcanoes, shield volcanoes and lava volcanoes.
Cinder Cones | Cinder cones are circular or oval cones made up of small fragments of lava from a single vent that have been blown into the air, cooled and fallen around the vent. |
Composite Volcanoes |
Composite volcanoes are steep-sided volcanoes composed of many layers of volcanic rocks, usually made from high-viscosity lava, ash and rock debris. Mt. Rainier and Mount St. Helens are examples of this type of volcano. |
Shield Volcanoes |
Shield volcanoes are volcanoes shaped like a bowl or shield in the middle with long gentle slopes made by basaltic lava flows. Basalt lava flows from these volcanoes are called flood basalts. The volcanoes that formed the basalt of the Columbia Plateau were shield volcanoes. |
Lava Volcanoes | Lava domes are formed when erupting lava is too thick to flow and makes a steep-sided mound as the lava piles up near the volcanic vent. The eruption of Mount St. Helens in 1980 was caused in part by a lava dome shifting to allow explosive gas and steam to escape from inside the mountain. |
What is the difference between lava and magma?
Magma is liquid rock inside a volcano. Lava is liquid rock (magma) that flows out of a volcano. Fresh lava glows red hot to white hot as it flows.
Thursday, October 30, 2014
Thank you! and New Test Date
Dear Parents,
Thank you for your generosity. Our fall basket was a huge success! Please make sure to check it out tonight.
Total value $625.00
(15) Gift cards totaling - $225.00 & (2) Gift certificates totaling - $400.00
$10.00 - Target
$10.00 - Target
$15.00 - Target
$20.00 - Target
$10.00 - Chick-fil-a
$10.00 - Chick-fil-a
$10.00 - Darden
$15.00 - Starbucks
$15.00 - iTunes
$15.00 - Bass Pro Shops
$20.00 - Sports Authority
$25.00 - Old Navy
$10.00 - Malco
$10.00 - Amazon
$30.00 - Amazon
I have postponed our solar system test until Friday, November 7th. This will allow the children to have more time to enjoy Fall Fest and more time for Mrs. Dixon and I to cover the stars.
Thank you for your generosity. Our fall basket was a huge success! Please make sure to check it out tonight.
(15) Gift cards totaling - $225.00 & (2) Gift certificates totaling - $400.00
$10.00 - Target
$10.00 - Target
$15.00 - Target
$20.00 - Target
$10.00 - Chick-fil-a
$10.00 - Chick-fil-a
$10.00 - Darden
$15.00 - Starbucks
$15.00 - iTunes
$15.00 - Bass Pro Shops
$20.00 - Sports Authority
$25.00 - Old Navy
$10.00 - Malco
$10.00 - Amazon
$30.00 - Amazon
I have postponed our solar system test until Friday, November 7th. This will allow the children to have more time to enjoy Fall Fest and more time for Mrs. Dixon and I to cover the stars.
Friday, October 24, 2014
Stars and Fall Fest
1. The star that is closest to the Earth is the sun.
2. A Star is a gigantic, glowing ball of plasma.
3. Stars are first formed as clouds of dust and gas.
4. Stars give off a tremendous amount of energy in the form of light and heat.
5. Most stars are between 1 billion and 10 billion years old.
6. Stars that have really strong gravity grow smaller over time and eventually turn into black holes.
7. The hottest stars give off a bluish light while the cooler stars give off a reddish light.
8. Stars seem to twinkle because their light travels through the earth’s atmosphere and the turbulence in the atmosphere affects the way stars are seen.
9. All the stars that make up the Milky Way Galaxy revolve around the center of the galaxy once every 200 million years or so.
10. The oldest star that has been discovered is HE 1523-0901, which is an estimated 13.2 billion years old.
3. Stars are first formed as clouds of dust and gas.
4. Stars give off a tremendous amount of energy in the form of light and heat.
5. Most stars are between 1 billion and 10 billion years old.
6. Stars that have really strong gravity grow smaller over time and eventually turn into black holes.
7. The hottest stars give off a bluish light while the cooler stars give off a reddish light.
8. Stars seem to twinkle because their light travels through the earth’s atmosphere and the turbulence in the atmosphere affects the way stars are seen.
9. All the stars that make up the Milky Way Galaxy revolve around the center of the galaxy once every 200 million years or so.
10. The oldest star that has been discovered is HE 1523-0901, which is an estimated 13.2 billion years old.
- Beautification Day is Saturday, October 25, from 8:30 a.m. to 12:30 p.m.
We will gratefully put to use donations of flats of blue and white pansies, bird seed, and other plant-related items... even if you can't come on Saturday. See wiki for more information.
- The theme of Family Gathering on October 24, is "Integrity" and will be led by Ms. Caldwell's class.
- Fall Fest is Thursday, October 30.
- We need donations of candy, 2 liter soft drinks and pre-packaged snack cakes. You may drop these items off at school in the boxes in the lobby beginning Tuesday morning.
- We need lots of volunteers! Please sign up here for at least one shift.
- Reminder: Fall Fest is only for Campus School families and students.
- Support Drive Jeans Day is Friday, October 31, for 100% participation of all families in the CSPN Support Drive.
- Family Gathering Helpers - If you would like to help Mrs. Bailey, please click on this wiki link It is a fun way to start your Friday!
- For more updates and reminders throughout the week you can find us on Facebook. Click here to like Campus School.
- School Supply Box Chair Opportunity
- We are looking for someone interested in taking over our school
supply box orders for the 2015-16 school year. Responsibilities for this
position begin in February 2015 and will continue through August.
Please email Kerry Shepard if you are interested or would like more information.
Monday, October 13, 2014
Inner and Outer Planets & Fall Fest Class Basket Information
Differences between the Inner and Outer Planets
Orbiting the Sun are eight planets. Despite all of these planets being different from each other, they can be put into two groups. One group contains the four planets closest to the Sun - Mercury, Venus, Earth and Mars. These are known as the Inner Planets or the Terrestrial Planets. The other group contains the four planets furthest from the Sun - Jupiter, Saturn, Uranus and Neptune. These are known as the Outer Planets or the Gas Giants. The two groups are separated by the Asteroid Belt, a region of thousands of asteroids in orbit of the Sun between Mars and Jupiter. Below is a table containing differences between the two groups of planets.Hello Everyone,
I hope you all are enjoying Fall break! This is a gentle reminder to please purchase gift cards for our class fundraiser basket and please send them in to the class by Friday, October 24th. You can get your gift card from where ever you choose ... any type, any place, and any amount! Please send them in an envelope addressed to Stacey Sheppard.
Thanks!
Stacey
Monday, September 29, 2014
Field Trip Change--Important Notice
Field Trip Change--Important Notice
Dear Parents,
After careful review of our field trip plans, we have determined
that the drive to our original destination, which is 2.5 hours one way,
will deeply impact the amount of time students would have to enjoy their
experience. There is also the possibility of inclement weather
Thursday night/early Friday morning. With those two things taken into
consideration, the 5th grade team has decided to change our destination
to Fort Pillow. Fort Pillow is located about 40 miles North of Memphis
along the Mississippi River. We have reserved the park's pavillion for
our use and plan to visit the museum and view the film provided by the
park. We also plan to take advantage of the many trails in the park.
Dr. Copeland has given permission for students to wear jeans, spirit
shirts (or uniform polos), and old tennis shoes (no sandals, Crocs, or
dress shoes) Friday for our trip.
We would like to ask parents to still meet at Campus by 7:30 in
order to avoid the arrival traffic and arrive at the park before 9:00.
Thank you so much for your understanding and cooperation with this. We
appreciate everything you do to help make Campus the wonderful place it
is.
Fort Pillow State Park — Tennessee State Parks
Located
on the western edge of Tennessee, approximately 40 miles north of
Memphis, Fort Pillow State Historic Park is rich in historic and
archaeological significance. Steep bluffs overlooking the Mississippi
River made this area a strategic location during the Civil War. The fort
was originally built by Confederate troops in 1861 and named after
General Gideon J. Pillow of Maury County. It was abandoned in 1862 due
to the Union Navy’s advancement along the Mississippi River. The area
became a state park in 1971. The 1,642 acre Fort Pillow is known for its
well-preserved breastworks and reconstructed inner fort. The park’s
museum offers Civil War artifacts including a canon and interpretive
displays relating to the history of Fort Pillow. There is a 12 minute
video on the 1864 Battle shown by request as well as tours of the museum
and restored fortifications. The museum is open from 8 a.m. – 4 p.m. Lunch is still provided! We will send home a map with where to meet by tomorrow.
Thursday, September 25, 2014
WHY PROJECT 1, Parent Teacher Conferences, and Field Trip
Jim Jaggers will be riding to our school on Wednesday Oct. 1. Along
with Jim we see other bicycle riders, a Go Jim Go pace car and a
WREG news van. Jim should arrive between 1:30-1:40, however this time frame does vary year to year.
Field Trip Permission Slip
Date: Friday, October 3, 2014
Time: 7:30 a.m.-2:45 p.m.
Activities: Visit Nathan Bedford Forrest State Park
Curriculum Connection: Students will visit a Civil War battle site that includes a museum, video presentation, and a hike to the highest elevation in West Tennessee.
Transportation: Parent drivers.
Cost: $5 per student—CASH ONLY, no cost for chaperons—All money is due Friday, September 26.
Lunch: Students will be given a picnic lunch at the park including hot dog (turkey dog), chips, drink, and cookie.
Chaperones: Mr. Stearnes, Mrs. Cordero, Mr. Shadow, and Ms. Fenney
Dear
Parents,
Thank you for returning the parent-teacher
conference sheets back to me so quickly. Many conferences are
scheduled back to back. Therefore it would be helpful if you could be in our
classroom at your scheduled time so that we may make the most out of our
discussion. If for any reason you cannot make your appointment please call me
at 678-2285. The master list may be viewed on the pages tab of our blog.
Why Project I
Due Date: September
29, 2014
A student may choose any area of
science that we have already covered this year. This is designed so the student
will investigate a question or topic to expand their knowledge. A student may
request a topic outside of this if they receive prior approval from me.
A student may choose how to share
their information. Examples are: poster, written report, PowerPoint, Prezi, video
demonstration, diorama, etc.
o
Student
must provide a specific question that they want answered by their project
presentation.
o
Student
must provide a minimum of three factual statements concerning their area of
study.
o
Spelling
counts!
o
Student
will provide a separate written five
paragraph summary (see rubric) that will contain a) a statement of their question, b) the facts provided, c)
the procedures they used in their quest for knowledge and d) a conclusion. This will be on a separate sheet from the presentation
material. You can view the rubric below for the written report and the project.
The project due date is Monday, September 29th, 2014. Field Trip Permission Slip
Date: Friday, October 3, 2014
Time: 7:30 a.m.-2:45 p.m.
Activities: Visit Nathan Bedford Forrest State Park
Curriculum Connection: Students will visit a Civil War battle site that includes a museum, video presentation, and a hike to the highest elevation in West Tennessee.
Transportation: Parent drivers.
Cost: $5 per student—CASH ONLY, no cost for chaperons—All money is due Friday, September 26.
Lunch: Students will be given a picnic lunch at the park including hot dog (turkey dog), chips, drink, and cookie.
Chaperones: Mr. Stearnes, Mrs. Cordero, Mr. Shadow, and Ms. Fenney
Thursday, September 18, 2014
Week 9- Nine Week Unit Test, The Fossil Record, and Go Jim Go/Coins 4 Kids
Coins 4 Kids
Monday, students will bring in pennies, Tuesday—nickels, Wednesday—dimes, Thursday—quarters and on Friday dollars will be collected.
Monday, students will bring in pennies, Tuesday—nickels, Wednesday—dimes, Thursday—quarters and on Friday dollars will be collected.
Students who bring in a dollar may wear jeans!
Go Jim Go is an annual event
that supports Le Bonheur Children's Hospital. Le Bonheur Children's
Hospital is a place for hope and healing for children and their families
across the Mid-South and beyond. More than 250,000
children are cared for annually at Le Bonheur Children's. With the
expertise of our physicians, medical team and state-of-the-art
technology, Le Bonheur Children's has the ability to care for the
community's sickest children.
Le Bonheur is a
not-for-profit hospital relying on the support of a generous community
to provide the best health care to all children. Our care and services
extend beyond the walls of Le Bonheur, providing many benefits
to the community. Our associates dedicate hours of tutoring and reading
in elementary schools, and our community outreach offers unique
programs that serve more than half a million children in the region. In
addition, Le Bonheur is recognized as one of the
nation's "Best Children's Hospitals" by U.S News and World Report.
Participating in Go Jim Go is
beneficial for students. Studies show youth who volunteer are more
likely to do well in school, graduate, become responsible adults and
continue being philanthropic throughout adulthood. Additionally,
students who participate in community service reported feeling better
about themselves and gaining respect and understanding for others. Go
Jim Go is an important community program, impacting the lives of youth
across the region.
The fossil record provides snapshots of the past that, when assembled,
illustrate a panorama of evolutionary change over the past four billion
years. The picture may be smudged in places and may have bits missing, but
fossil evidence clearly shows that life is old and has changed over time
Nicholas Steno's anatomical drawing of an extant shark (left) and a fossil
shark tooth (right). Steno made the leap and declared that the fossil teeth
indeed came from the mouths of once-living sharks.
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