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Going on a virtual tour: use these photos to complete assignment to the left.

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Assignment #32  continued Textbook page B69

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Assignment #32  continued Textbook page B69

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Directions: Complete #1 - #5

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Assignment # 28 Contour Map Lesson Notes

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Assignment # 28 Contour Map Lesson Notes

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Directions: Take notes of most important information from the Topographic Maps Powerpoint

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6th Grade Science - Student Assignments Begin Here:  ***Assignments are numbered here the same way they are in Powerschool Gradebook.  Continue scrolling to the right to see more.

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6th Grade Science - Student Assignments Begin Here:  ***Assignments are numbered here the same way they are in Powerschool Gradebook.  Continue scrolling to the right to see more.

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Most of these beginning assignments involve setting up the interactive science notebook.

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Use this template to write out vocabulary words

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Assignment #26 Earth Unit Essential  Vocabulary Words

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Assignment #26 Earth Unit Essential  Vocabulary Words

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Directions:  Glue the list of words and definitions into  notebook on a left page
THEN.... use the Frayer model template to analyze 8 words on the facing right page (one word per template)

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this row

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Directions:  Write both reflections in your notebook.
Reflection 1:  Write 5 facts about safety in your notebook
Reflection 2: List the steps of the scientific method in your notebook

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Assignments #18 & 19 Scientific Method Study Guide

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Assignments #18 & 19 Scientific Method Study Guide

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Directions: Get sheets from class (2 sheets). Complete study guide sheets and glue into notebook

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Assignment #17 Compare Independent & Dependent Variables.                        Directions:   Write a reflection in your notebook.  Explain the difference between an Independent Variable and a Dependent Variable.            

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Assignment #17 Compare Independent & Dependent Variables.                        Directions:   Write a reflection in your notebook.  Explain the difference between an Independent Variable and a Dependent Variable.            

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Give examples of each

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Assignment #16 Identifying Variables  & Identifying Constants

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Assignment #16 Identifying Variables  & Identifying Constants

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Directions: Get handout from class. Complete the front and back of the sheet and glue it into notebook so both sides can be seen (glue just across top)

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Directions: Complete the lab using the steps in the sheet pictured below (lab was done in class) Turn sheet into teacher.

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Assignment #11  Safety Test Scantron Results Sheet

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Assignment #11  Safety Test Scantron Results Sheet

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Directions: Glue your safety test scantron sheet onto this page

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Directions: On the next blank page in your notebook,  illustrate 1 safety rule and write the rule at the bottom of your paper.

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Assignment #9    Assignment Removed ... Do NOT Complete.

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Assignment #9    Assignment Removed ... Do NOT Complete.

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I removed this assignment from the grades.

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Assignment #8 Spongebob Science Safety Rules

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Assignment #8 Spongebob Science Safety Rules

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Directions: Read the passage and underline all the broken safety rules. Glue sheet into notebook

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Assignment #7     Sheet 2 - What not to do:  laboratory safety ANSWERS / Key to pictures in first sheet      

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Assignment #7     Sheet 2 - What not to do:  laboratory safety ANSWERS / Key to pictures in first sheet      

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Directions: Glue sheet into notebook

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Assignment #7      Sheet 1 -  What not to do:  laboratory safety

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Assignment #7      Sheet 1 -  What not to do:  laboratory safety

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Directions: Glue sheet into notebook

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Assignment #6       Flinn Safety Contract

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Assignment #6       Flinn Safety Contract

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Directions:  Students and Parents should both  complete signature part and questions at bottom of sheet and glue in notebook

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Directions: Glue in notebook

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Lampkin's Copy of 6th Grade Syllabus Page 1 2019 (1)

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Assignment #4             Interactive Notebook Rubric

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Assignment #4             Interactive Notebook Rubric

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Directions:  Get rubric handout from class. Glue page in notebook.

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Assignments 2&3        Interactive Notebook Guide (2 parts when cut in half)

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Assignments 2&3        Interactive Notebook Guide (2 parts when cut in half)

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Topic:  What to expect when using interactive notebooks.
Directions: Cut in half and glue in notebook. Get handout from class.

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Assignment #1                        All about me

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Assignment #1                        All about me

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Directions: Write student name, hobbies and people they can rely on for support.

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Interactive Notebook pages. Start here for the notebook organization 

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Interactive Notebook pages. Start here for the notebook organization 

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Students should number all the pages front and back in their notebook

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Assignment #31  Page 3 of 3 continued          Contour Map Practice

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Assignment #31  Page 3 of 3 continued          Contour Map Practice

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Directions: Complete and glue into notebook 9/26

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Assignment #31  Page 2 of 3 continued        Contour Map

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Assignment #31  Page 2 of 3 continued        Contour Map

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Directions:  Complete and glue into notebook
9/26

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Assignment #31 Page 1 of 3 Contour Maps Handout

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Assignment #31 Page 1 of 3 Contour Maps Handout

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Directions: Complete and glue into notebook
9/26

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9/26

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IXL | Select parts of a topographic map | 6th grade science

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Improve your science knowledge with free questions in "Select parts of a topographic map" and thousands of other science skills.

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Contour Maps Lesson PPT - Lesson Resource

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Contour Maps Lesson PPT - Lesson Resource

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9/23 -24

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not yet assigned

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Animation of where the largest earthquakes of the past 100 years have struck

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brief video 2:36

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Teacher's Guide 9/25

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Code is 897138
Use your real names

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Free gamified quizzes on every subject that students play in class and at home. Pick an existing quiz or create your own for review, formative assessment, and more.

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Lesson Resource

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Experiments Archived | Science Experiments | Steve Spangler Science

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For more than 25 years Steve Spangler Science has been bringing FUN to science, with these popular items!

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Lesson Resource

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With this science-magic trick, you'll put a new spin on our famous Density Column demonstration. First, you'll discover how to stack nine layers of liquids on top of each other. That alone looks really cool, but then you take it up a notch by making different solid objects "float" in the middle of all those cool looking stacked liquids. You'll surprise yourself and your friends with what you can do with the 9-Layer Density Tower.

Experiment Materials

Liquid Materials, 1.5 to 3.5 oz (50 to 100 ml) of each:

Honey

Corn Syrup

100% Maple Syrup

Whole Milk

Dish Soap

Water

Vegetable Oil

Rubbing Alcohol

Lamp Oil

Other Materials:

1 Quart (1L) container - tall, narrow, clear

9, 4 oz (118 ml) plastic cups

Turkey baster

Food coloring

Metal bolt

Popcorn kernel

Board game die

Cherry tomato

Plastic beads

Plastic soda cap

Ping-Pong™ ball

How Does It Work

Density is basically how much "stuff" is packed into a particular volume. It's a comparison between an object's mass and its volume. Remember the all-important equation: density = mass ÷ volume. Based on this equation, if the weight (or mass) of something increases but the volume stays the same, then density goes up. Likewise, if the mass decreases but the volume stays the same, then density goes down. Lighter liquids (like water or vegetable oil) are less dense than heavier liquids (like honey or corn syrup) so they float on top of the heavier liquids. The same amount of two different liquids you used in the container will have different densities because they have different masses. The liquids that weigh more (a higher density) will sink below the liquids that weigh less (a lower density).

To test this, you might want to set up a sensitive kitchen scale and weigh each volume of the liquids that you added to the column. Make sure that you weigh identical volumes of each liquid. You should find that the weights of the liquids correspond to each different layer of liquid. For example, the honey will weigh more than the dish soap. By weighing the same volume (e.g. ¼ cup, 60 ml) of these liquids, you will find that density and weight are closely related.

By convention, plain water has a density of 1.0 and that's measured in g/cm ³ or g/ml. So, a cubic centimeter of water has a mass of 1 gram and fills 1 milliliter of volume. If a substance has a density less than 1.0 g/cm ³, it floats on water and one with a density more than 1.0 g/cm ³, it sinks in water. The numbers below are based on data from manufacturers for each item. Since each manufacturer has its own "secret" formula, densities may vary slightly from brand to brand for the same product but these are pretty close.

The same rule for "sink or float" goes for the small objects that you dropped into your density column. The metal bolt is more dense than all of the liquids in the column and therefore sinks directly to the bottom. Less dense objects will float on individual layers up the column. For instance, the plastic beads are more dense than the vegetable oil and everything above it but less dense than the water and everything below it. This makes the beads settle on top of the water. The Ping-Pong ball is the least dense of it all and floats on top.

Take It Further

This is the perfect opportunity to get in some scientific exploration. Use what you learned from dropping the beads, soda bottle cap, tomato, and game die into the container to figure out which items are more or less dense than water. Which items have more density than vegetable oil? What items are less dense than honey? You could make a hypothesis about the density of an object and then test it in the column. How do the data support or not support the results?

When all the liquids and small objects have been added to your density tower, you will have what appears to be a "magic" column but it's all based on science. All of the liquids will be clearly distinguishable from each other and each of the objects will have settled at different levels within the column. Construct a table to show the order that the liquids and objects are in at the start. Be sure to record the date, too. If you leave it undisturbed over time, some interesting changes may occur in the column. Keep track of what you see with notes and photos with dates. Science fair anyone?

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Amazing 9 Layer Density Tower - SICK Science! | Science Experiments | Steve Spangler Science

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With this science-magic trick, you'll put a new spin on our famous Density Column demonstration. First, you'll discover how to stack nine layers of liquids on top of each other. That alone looks really cool, but then you take it up a notch by making different solid objects "float" in the middle of all those cool looking stacked liquids.

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use to measure the marble's mass

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Please click here if you are not redirected within a few seconds.

Press the "ON" button and wait for the balance to show zeroes on the digital screen. Use tongs or gloves to place the empty container you will use for the substance to be measured on the balance platform. Fingerprints and other greases from your hands add mass and must be avoided for accurate measurements.

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how to use an electronic balance - Google Search

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Please click here if you are not redirected within a few seconds. Place the electronic balance on a flat, stable surface indoors. The precision of the balance relies on minute factors and wind, shaky surfaces, or similar forces will cause the readings to be inaccurate.

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How to use a Triple Beam Balance Lesson 

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How to use a Triple Beam Balance Lesson 

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Please click here if you are not redirected within a few seconds.

To find out the weight of the object, you'll need to slide the weight poises until the pointer is at zero again. Start with the two heavier weight poises and then use the lightest one to do the fine tuning. Our triple beam balance and the Ohaus triple beam balance are accurate to 0.1 grams.

Sep 14, 2011 · Hate to be a 2nd grader here but what is the answer to the empty beaker & the one filled with ...Duration: 6:00 Posted: Sep 14, 2011

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how to use a triple beam balance step by step - Google Search

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Please click here if you are not redirected within a few seconds. To find out the weight of the object, you'll need to slide the weight poises until the pointer is at zero again. Start with the two heavier weight poises and then use the lightest one to do the fine tuning.

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Assignment #24  9/16/19              Science RUNNERS Day

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Assignment #24  9/16/19              Science RUNNERS Day

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Directions: Use the RUNNERS strategy to read the article and questions and to answer the questions. Glue the article into your notebook.

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Assignment #27 Density Column Lab Part 1

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Assignment #27 Density Column Lab Part 1

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Directions: Complete the sheet by showing your work for each step of the lab

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Understanding density has never been easier or more colorful! The Sugar Rainbow is a creative and engaging way to see how liquids of different densities stack on top each other. There's an additional lesson about adhesion and cohesion in the mix for you, too. A simple combination of some sugar and water with vivid colors leads to an awesome science experience about density.

Experiment

Fill each of the six glasses with water. NOTE: The glasses need to be stable and about as deep as the straw is long. As you fill the straw with solutions, it has to be plunged deeper and deeper into the liquids.

Use coloring tablets or food coloring to dye the water a different, bright color in each glass. Stir it completely.

The first of the six glasses will be just colored water with no sugar. The second color receives one rounded teaspoon of sugar. The third color receives two rounded teaspoons of sugar. The fourth gets three teaspoons and so on to five teaspoons of sugar in the last glass. Stir the solution in each glass until the sugar is completely dissolved. NOTE: Using warm or room temperature water will speed up this process.

Grab the straw and, if you haven't already, remove the wrapper. Hold the straw near one end, wrapping four fingers around the straw and placing your thumb over the straw's top opening. To make your Sugar Rainbow, lift your thumb off the opening, dunk the lower end of the straw about 1" (3 cm) into the plain water. Cap the straw firmly with your thumb, lift it out of the water, and dip it quickly into the 1 tsp solution. This time, go a little deeper than you did into the first glass. You want the layers to be about the same thickness. With the straw in the liquid, lift your thumb but quickly replace it. Lift the straw and you'll have the first and second colored solutions in a stack inside the straw. Continue the dipping process until you have all six colored solutions inside the straw. It's a density column of sugar water, a Sugar Rainbow!

When you're ready, hold the straw over the dish and lift your thumb to empty the straw. Rinse it and make another one.

How Does It Work

Density is the measurement of how much "stuff" is packed into a measured space. That's how we get the equation for density: Density = Mass (the stuff) ÷ Volume (a measured space). Nearly every substance and material imaginable has a different density. This is especially true for the six solutions you made using sugar and water.

By increasing the amount of sugar in the solution but keeping the amount of water constant, you create solutions that have increasing densities. The more sugar that's mixed into a measured amount of water, the higher the density of the mixture. As the Sugar Rainbow reveals, a solution with a low density stacks on top of a mixture with a high density.

So, density explains why the solutions stack on top of each other inside the straw, but what keeps the solutions in the straw? You could expect them to just pour out of the straw as you lift the straw from a solution. However, thanks to cohesion (similar molecules attracting each other) and adhesion (different molecules attracting each other), there is surface tension sealing the water at the bottom of the straw. The surface tension is strong enough to help hold the solutions in the straw... as long as air pressure inside the straw is lower than the air pressure outside the straw. Gravity tugs the solutions downward which creates a slight vacuum in the empty part of the straw. That lowers the air pressure inside the straw which is why you need your thumb to cap the straw. This prevents air pressure from equalizing inside the straw. Remove your thumb, air pressure equalizes, and gravity simply moves the colored solutions out.

Take It Further

Use a turkey baster as a replacement for the straw to slowly layer the colored sugar solutions into a larger glass to create an even bigger rainbow. Hold the tip of the baster against the side of the container close to the surface of the liquid already in the glass. Squeeze the baster gently so the water flows slowly down the side of the container and then onto the previous layer. If you try to rush it, the layers will just mix together. Rinse the baster between each layer. Move the baster upward on the side of the glass as needed so it doesn't touch the surface of the solution. Layer all the sugar solutions in the same way. This can be hard to do but it's worth the effort when you finish. Get some pictures!

Fun Fact

A dramatic salt water density change can be experienced in real life. While humans will (sort of) float in an ocean, they really float in bodies of water like Utah's Great Salt Lake and the Dead Sea in Israel and the West Bank. They are so salty that it's nearly impossible to sink in them! Just be sure to rinse off really well when you get out.

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Sugar Rainbow | Experiments | Steve Spangler Science

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Understanding density has never been easier or more colorful! The Sugar Rainbow is a creative and engaging way to see how liquids of different densities stack on top each other. There's an additional lesson about adhesion and cohesion in the mix for you, too.

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Density Video Resource

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Experiments Archived | Science Experiments | Steve Spangler Science

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For more than 25 years Steve Spangler Science has been bringing FUN to science, with these popular items!

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Assignment #25 Crossword Puzzle Earth Vocabulary

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Assignment #25 Crossword Puzzle Earth Vocabulary

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Directions:  Students will use the Earth Unit Essential Vocabulary words to create their own crossword puzzle in their notebook.  Create the puzzle on the left page, put answers on the facing  right page.

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9/12/19 Notebook Organization Check on this day

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9/12/19 Notebook Organization Check on this day

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All pages are glued down

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Assignment #22 Teacher Notes Lesson Resource

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Assignment #22 Teacher Notes Lesson Resource

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Use to help with student notes

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Assignment #23 Lesson Resource 9/11/19 Quizlet

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Assignment #23 Lesson Resource 9/11/19 Quizlet

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Directions:  Use quizlet to help color and label the layers of the Earth.

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Start studying Layers of the Earth. Learn vocabulary, terms, and more with flashcards, games, and other study tools.

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Assignment #23 Earth's Layers Analogy Student Practice Coloring

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Assignment #23 Earth's Layers Analogy Student Practice Coloring

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Directions:  Color and Label the layers of the Earth. Use the quizlet site to help, Glue sheet into notebook

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The Lithosphere-asthenosphere boundary ( LAB) represents a mechanical difference between layers in Earth's inner structure. Earth's inner structure can be described both chemically ( crust, mantle, core) and mechanically. The Lithosphere-asthenosphere boundary (referred to as the LAB by geophysicists) lies between Earth's cooler, rigid lithosphere and the warmer, ductile asthenosphere. The actual depth of the boundary is still a topic of debate and study, although it is known to vary according to the environment.

Defining the LAB

The LAB is determined from the differences in the lithosphere and asthenosphere including, but not limited to, differences in grain size, chemical composition, thermal properties, and extent of partial melt; these are factors that affect the rheological differences in the lithosphere and asthenosphere.

The LAB separates the mechanically strong lithosphere from the weak asthenosphere. The depth to the LAB can be estimated from the amount of flexure the lithosphere has undergone due to an applied load at the surface (such as the flexure from a volcano). Flexure is one observation of strength, but earthquakes can also be used to define the boundary between "strong" and "weak" rocks. Earthquakes are primarily constrained to occur within the old, cold, lithosphere to temperatures of up to ~650°C. This criterion works particularly well in oceanic lithosphere, where it is reasonably simple to estimated the temperature at depth based upon the age of the rocks. The LAB is most shallow when using this definition. The MBL is rarely equated to the lithosphere, as in some tectonically active regions (e.g. the Basin and Range Province) the MBL is thinner than the crust and the LAB would be above the Mohorovičić discontinuity.

The definition of the LAB as a thermal boundary layer (TBL) comes not from temperature, but instead from the dominant mechanism of heat transport. The lithosphere is unable to support convection cells because it is strong, but the convecting mantle beneath is much weaker. In this framework, the LAB separates the two heat transport regimes [ conduction vs. convection]. However, the transition from a domain that transports heat primarily through convection in the asthenosphere to the conducting lithosphere is not necessarily abrupt and instead encompasses a broad zone of mixed or temporally variable heat transport. The top of the thermal boundary layer is the maximum depth at which heat is transported only by conduction. The bottom of the TBL is the shallowest depth at which heat is transported only by convection. At depths internal to the TBL, heat is transported by a combination of both conduction and convection.

The LAB is a rheological boundary layer (RBL). Colder temperatures at Earth's shallower depths affect the viscosity and strength of the lithosphere. Colder material in the lithosphere resists flow while the "warmer" material in the asthenosphere contributes to its lower viscosity. The increase in temperature with increasing depth is known as the geothermal gradient and is gradual within the rheological boundary layer. In practice, the RBL is defined by the depth at which the viscosity of the mantle rocks drops below ~ .[4]

However, mantle material is a Non-Newtonian fluid, i.e. its viscosity depends also on the rate of deformation. It means that LAB can change its position as a result changes of the stresses.

Another definition of the LAB involves differences in composition of the mantle at depth. Lithospheric mantle is ultramafic and has lost most of its volatile constituents, such as water, calcium, and aluminum. Knowledge of this depletion is based upon the composition of mantle xenoliths. The depth to the base of the CBL can be determined from the amount of forsterite within samples of olivine extracted from the mantle. This is because partial melting of primitive or asthenospheric mantle leaves behind a composition that is enriched in magnesium, with the depth at which the concentration of magnesium matches that of the primitive mantle being the base of the CBL.

Measuring the LAB depth

Seismic observations

The seismic LAB (i.e. measured using seismological observations) is defined by the observation that there exists seismically fast lithosphere (or a lithospheric lid) above a low-velocity zone (LVZ). Seismic tomographic studies suggests that the LAB is not purely thermal, but rather is affected by partial melt. The cause of the LVZ could be explained by a variety of mechanisms. One way to determine if the LVZ is generated by partial melt is to measure the electrical conductivity of the Earth as a function of depth using magnetotelluric (MT) methods. Partial melt tends to increase conductivity, in which case the LAB can be defined as a boundary between the resistive lithosphere and conductive asthenosphere.

Because mantle flow induces the alignment of minerals (such as olivine) to generate observable anisotropy in seismic waves, another definition of the seismic LAB is the boundary between the anisotropic asthenosphere and the isotropic (or a different pattern of anisotropy) lithosphere.

The seismic LVZ was first recognized by Beno Gutenberg, whose name is sometimes used to refer to the base of the seismic LAB beneath oceanic lithosphere. The Gutenberg discontinuity coincides with the expected LAB depth in many studies and has also been found to become deeper under older crust, thus supporting the suggestion that the discontinuity is closely interrelated to the LAB. Evidence from converted seismic phases indicates a sharp decrease in shear-wave velocity 90-110 km below continental crust. Recent seismological studies indicate a 5 to 10 percent reduction in shear-wave velocity in the depth range of 50 to 140 km beneath ocean basins.

Beneath oceanic lithosphere

Beneath oceanic crust, the LAB ranges anywhere from 50 to 140 km in depth, except close to mid-ocean ridges where the LAB is no deeper than the depth of the new crust being created. Seismic evidence shows that oceanic plates do thicken with age. This suggests that the LAB underneath oceanic lithosphere also deepens with plate age. Data from ocean seismometers indicate a sharp age-dependent LAB beneath the Pacific and Philippine plates and has been interpreted as evidence for a thermal control of oceanic-lithosphere thickness.

Beneath continental lithosphere

The continental lithosphere contains ancient, stable parts known as cratons. The LAB is particularly difficult to study in these regions, with evidence suggesting that the lithosphere within this old part of the continent is at it thickest and even appears to exhibit large variations in thickness beneath the cratons, thus supporting the theory that lithosphere thickness and LAB depth are age-dependent. The LAB beneath these regions (composed of shields and platforms) is estimated to be between 200 and 250 km deep. Beneath Phanerozoic continental crust, the LAB is roughly 100 km deep.

References

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The Lithosphere-asthenosphere boundary ( LAB) represents a mechanical difference between layers in Earth's inner structure. Earth's inner structure can be described both chemically ( crust, mantle, core) and mechanically. The Lithosphere-asthenosphere boundary (referred to as the LAB by geophysicists) lies between Earth's cooler, rigid lithosphere and the warmer, ductile asthenosphere.

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Assignment #22 Lesson Resource 9/11/19  Video  Journey to the center of the Earth Trailer  2:15 

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Assignment #22 Lesson Resource 9/11/19  Video  Journey to the center of the Earth Trailer  2:15 

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Directions:  View the video clip to help with Assignment #22 guided notes.

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Edpuzzle video lesson. Make any video your lesson. Take a video and crop it, add your voice or embed questions at any point.

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Assignment #22 Layers of the Earth Student Notes

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Assignment #22 Layers of the Earth Student Notes

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Directions: Use information from the Powerpoint and video to complete the notes page. Glue page into notebook

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Assignment #22 Lesson Resource 9/11/19  Layers of the Earth Powerpoint

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Assignment #22 Lesson Resource 9/11/19  Layers of the Earth Powerpoint

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Directions: View Powerpoint to help you with Assignment 22 guided notes

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Week of 9/9-13/2019

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Assignments #14 & 15 Part 2               Scientific Method Controls and Variables (Spongebob)

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Assignments #14 & 15 Part 2               Scientific Method Controls and Variables (Spongebob)

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Directions: Complete the sheet using the directions listed at the top. Glue sheet into notebook

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Assignments #14 & 15  Part 1               Scientific Method  Controls and Variables (Spongebob) 

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Assignments #14 & 15  Part 1               Scientific Method  Controls and Variables (Spongebob) 

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Directions: Complete each section of the sheet using directions listed. Glue sheet into notebook

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Week of 9/2-6/19

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You've discovered a problem with the crime scene photos
from a recent case.
Someone has tampered with your crime scene!

See how many differences you can spot between two photographs
of the same crime scene.

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You've discovered a problem with the crime scene photos from a recent case.Someone has tampered with your crime scene! See how many differences you can spot between two photographs of the same crime scene.

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9/3/18 Eye Witness Basics Students Notes Page

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9/3/18 Eye Witness Basics Students Notes Page

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Scientific Method Notes guide for students

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Scientific Method Notes guide for students

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Lab: How many drops of water fit on a penny? 

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Lab: How many drops of water fit on a penny? 

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There's a scientific method to Tim and Moby's madness! Learn about observation, experimentation--and oh, those heady conclusions!

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Scientific Method for Kids | Learn all about the Scientific Method Steps

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Assignment #12 Scientific Method Graphic Organizer

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Assignment #12 Scientific Method Graphic Organizer

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Directions:  Fill in the blanks to complete the sentences and steps in the organizer.  Glue sheet into notebook.
(Answers at the end to help you)

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8/29/19 Flinn Science Safety Test Answers

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8/29/19 Flinn Science Safety Test Answers

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8/28/19 Create your own safety poster. Examples

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8/28/19 Create your own safety poster. Examples

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Samples

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pinterest.com
Make a Science Fair Project about science safety: Lab Safety ...
790 × 1000 - 124k - jpg

pinterest.com
Science Lab Safety is very important! | Poster Ideas | Science lab ...
1584 × 2016 - 619k - png

artskills.com
Make a Science Fair Project | Poster Ideas - Science Safety Rules ...
790 × 1000 - 126k - jpg

artskills.com
Make a Science Fair Project About Science Lab Safety | Science Lab ...
790 × 1000 - 105k - jpg

pinterest.com
Pinterest
400 × 566 - 45k - jpg

msperezrocketscience.w...
Science Lab Safety (8-15-18) - Ms. Perez Science-Biotechnology
236 × 275 - 18k - jpg

teacherspayteachers.com
original-869465-1.jpg
350 × 271 - 52k - jpg

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science safety poster ideas - Google Search

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pinterest.com Make a Science Fair Project about science safety: Lab Safety ...790 × 1000 - 124k - jpg pinterest.com Science Lab Safety is very important!

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6th Grade Science:  1st Row - RESOURCES:  Powerpoints, Video clips,  Images and Some Handouts                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                              ** See following rows for STUDENT ASSIGNMENTS                              

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6th Grade Science:  1st Row - RESOURCES:  Powerpoints, Video clips,  Images and Some Handouts                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                              ** See following rows for STUDENT ASSIGNMENTS                              

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use with handout