PES Skill Sheets.book - Capital High School

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Page 2 of 4 Two other continents are important to our story. They are called Baltica and Laurentia. At the center of Laurentia was a core piece that was very old even then. This core piece is called the craton. The craton had been changed again and again, but it was stable inside Laurentia. Today the craton of Laurentia forms the central United States. You may wonder where these names came from. After all, these continents were gone many millions of years before humans appeared on Earth. They are modern names proposed and adopted by geologists. The first collision Rifting and subduction caused Baltica to move in a jerky path. Eventually, Baltica collided with Laurentia to form a larger combined continent. This new continent is called Laurasia. A high mountain range formed where the colliding continents made contact. This mountain range lay deep inside Laurasia. Today the remains of this high mountain range form our northern Appalachian Mountains. Gondwanaland collides Subduction continued to bring continents together. Next mighty Gondwanaland was drawn ever closer to Laurasia. Gondwanaland collided just below where Laurentia and Baltica collided with each other. This new collision raised another set of mountains that continued the northern Appalachians into what are now the southern Appalachians. The combined Appalachians were as high as the Himalayans of today! The super continent Pangaea was then complete and the lofty Appalachian Mountains stood near its center. Pangaea breaks up Pangaea did not remain together for very long, only a few tens of millions of years. The same rifting process that broke up Rodinia split the new super continent into smaller pieces. Our future East Coast had been deep inside the central part of Pangaea. But in the break-up, a rift valley split our eastern shore away from what is now Africa. Instead of an inland place, our East Coast became an eastern shore. The East Coast after Pangaea One of the amazing things in geology is how quickly mountain ranges are eroded away. After Pangaea broke up, the Appalachians completely eroded away. All that was left was a flat plain! The sediments produced from this erosion formed deep layers on the eastern shore and near-shore waters. These coastal margin sediments make up most of the eastern states today. But wait a minute; today we see rounded mountains where there had been only flat plains. What formed the rounded Appalachian Mountains of today? 19.4
Page 3 of 4 When a mountain is formed, some of it is pressed deep into the mantle by the weight of the mountain above. It’s like stacking wood blocks in water. As the stack grows taller, it also sinks deeper. Erosion 19.4 takes a tall mountain down quickly. With the top gone, its bottom rebounds back to the surface. In this way, the Appalachian Mountains that we see today are actually the rebounded lower section of the mountains that once had been pressed deep below Earth’s surface. The West Coast and the Ancestral Rocky Mountains There are two Rocky Mountain ranges. The first is called the Ancestral Rocky Mountains. The Ancestral Rocky Mountains were formed when subduction caused an ancient collision with Laurentia. The collision struck Laurentia on the side that would become our western states. In other words, the Ancestral Rocky Mountains already existed before Pangaea formed. The Ancestral Rockies were then heavily weathered and the sediment deposited on the surrounding plains. Today the Front Range of Colorado is part of the exposed remains of the Ancestral Rocky Mountains. Pangaea and the West Coast Our West Coast did not exist as Pangaea began to break up. The shoreline was near the present eastern border of California. What would become our West Coast states were sediments and islands scattered in the ocean to the west. North America began to move westward as it was rifted apart from Pangaea. A subduction zone appeared in front of the moving continent. As the ocean floor dove under the westwardmoving continent, these sediments, islands and even pieces of ocean floor became permanently attached to the continent. Our western shore grew in this way, forming the shape that we see today. The modern Rocky Mountains The mid-ocean ridge that was forming the subducting ocean plate was not too far away to the west. As the plate subducted, the mid-ocean ridge got closer and closer to the edge of the continent. This changed the way that the plate subducted. The result was that stronger push pressure caused the continent to buckle well back from its edge. In this way, the modern Rocky Mountains were formed near the remains of the Ancestral Rocky Mountains.
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Chapter and Section Chapter 1: Meas
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Chapter and Section Chapter 5: Forc
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Chapter and Section Chapter 9: Heat
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Chapter and Section Chapter 14: Cha
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Chapter and Section Chapter 18: Ear
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Chapter and Section Chapter 24: Wav
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Name: Date: 1.1 Lab Safety What can
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Page 3 of 6 Safety quiz 1. Draw a d
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Page 5 of 6 c. You suddenly you beg
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Name: Date: 1.1 Using Your Textbook
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Page 2 of 3 The following prefixes
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Name: Date: 1.1 Scientific Notation
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Page 3 of 3 3. Write the numbers in
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Page 2 of 4 Example 1: Measuring ob
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Page 4 of 4 4. . Prefix Symbol Mult
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Name: Date: 1.2 Reading Strategies
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Name: Date: 1.2 Stopwatch Math What
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Name: Date: 1.2 Understanding Light
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Name: Date: 1.2 Indirect Measuremen
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Name: Date: 1.3 Dimensional Analysi
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Name: Date: Skill Builder Fractions
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Page 3 of 4 Solving fraction proble
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Name: Date: 1.3 Significant Digits
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Page 3 of 4 Follow these steps for
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Name: Date: 1.3 Study Notes This sk
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Name: Date: 1.3 Science Vocabulary
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Page 3 of 3 Using the table of pref
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Page 2 of 2 5. Earth’s moon is co
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Page 2 of 3 When precise conversion
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Name: Date: 1.4 Creating Scatterplo
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Page 3 of 3 g. What is the position
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Page 2 of 2 1.4 1. Given the variab
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Page 2 of 3 Step 3: Look at the ran
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Name: Date: 1.4 Recognizing Pattern
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Page 3 of 3 Answer the following qu
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Page 2 of 2 4. Measurements: List a
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Page 2 of 2 2. Your teacher shows y
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Page 2 of 4 Recording valid observa
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Page 4 of 4 b. How did the student
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Page 2 of 3 Name: Lucy O. Date: Jan
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Name: Date: 2.2 Using Computer Spre
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Page 3 of 3 5. The following data i
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Page 2 of 2 2. John notices that hi
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Name: Date: 3.1 Latitude and Longit
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Page 3 of 4 Use an atlas or globe t
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Name: Date: 3.1 Map Scales Mapmaker
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Page 3 of 3 f. Point Q to Point M g
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Page 2 of 5 It’s time to go! 3.1
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Page 4 of 5 37. Now you will head t
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Name: Date: 4.1 Vectors on a Map Yo
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Page 2 of 3 1. Draw a profile map o
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Name: Date: 3.3 Bathymetric Maps Im
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Page 1 of 2 3.3 Tanya Atwater Tanya
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Name: Date: 4.1 Solving Equations w
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Page 3 of 4 Use the formula V = l
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Name: Date: 4.1 Problem Solving Box
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Page 2 of 3 In problems 6 and 7, yo
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Name: Date: 4.1 Percent Error When
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Page 3 of 3 1. The lab group conduc
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Page 2 of 3 1. A bicyclist travels
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Name: Date: 4.1 Velocity Speed and
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Name: Date: 4.2 Calculating Slope f
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Name: Date: 4.2 Analyzing Graphs of
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Page 3 of 4 1. For each position-ti
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Name: Date: 4.2 Analyzing Graphs of
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Name: Date: 4.3 Acceleration Accele
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Name: Date: 4.3 Acceleration and Sp
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Page 3 of 3 3. Graph 3: 4. Find acc
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Page 2 of 3 Example 1: How fast wil
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Name: Date: 5.1 Ratios and Proporti
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Name: Date: 5.1 Internet Research S
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Name: Date: 5.1 Preparing a Bibliog
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Name: Date: 5.1 Mass vs. Weight Wha
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Page 2 of 2 1. A physical science t
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Page 2 of 2 How much does it weigh
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Page 2 of 2 Answer the following pr
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Name: Date: 5.3 Equilibrium When al
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Name: Date: 6.1 Net Force and Newto
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Page 2 of 2 Reading reflection 1. I
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Name: Date: 6.3 Applying Newton’s
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Name: Date: 6.3 Momentum Conservati
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Name: Date: 6.3 Collisions and Cons
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Name: Date: 6.3 Rate of Change of M
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Page 3 of 3 6. A 50.-g (0.050-kg) e
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Page 2 of 2 1. A machine uses an in
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Page 2 of 2 Example 3: A 500-newton
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Page 2 of 2 7. You pull your sled t
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Page 2 of 2 The relationship betwee
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Page 2 of 2 6. Use the gear ratio f
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Page 2 of 2 The three classes of le
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Page 2 of 2 3. Now, calculate the g
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Page 2 of 2 To do this calculation,
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Name: Date: 7.2 Energy Transformati
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Name: Date: 7.2 Conservation of Ene
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Page 2 of 2 Reading reflection 1. W
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Name: Date: 7.3 Power In science, w
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Name: Date: 7.3 Power in Flowing En
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Name: Date: 7.3 Efficiency and Ener
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Page 2 of 2 Reading the temperature
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Page 2 of 4 1. For each of the prob
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Page 4 of 4 1. Surface temperatures
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Page 2 of 2 The graph below shows a
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Name: Date: 9.1 Using the Heat Equa
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Name: Date: 10.1 Measuring Mass wit
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Page 3 of 3 Reading the balance cor
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Page 2 of 2 d. Explain how the disp
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Page 2 of 3 Calculating volume of a
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Name: Date: 10.1 Density The densit
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Name: Date: 10.3 Pressure in Fluids
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Name: Date: 10.3 Boyle’s Law The
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Name: Date: 10.4 Charles’s Law Ch
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Name: Date: 10.4 Archimedes 10.4 Ar
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Name: Date: 10.4 Narcís Monturiol
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Name: Date: 10.4 Archimedes’ Prin
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Name: Date: 11.1 Layers of the Atmo
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Page 2 of 2 Reading reflection 1. H
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Page 2 of 3 Using temperature data
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Page 1 of 2 11.3 Joanne Simpson 11.
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Name: Date: 11.3 Weather Maps You h
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Name: Date: 11.3 Tracking a Hurrica
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Page 3 of 4 Hurricane Andrew crosse
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Name: Date: 12.1 Structure of the A
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Name: Date: 12.1 Atoms and Isotopes
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Name: Date: 12.1 Ernest Rutherford
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Name: Date: 12.2 Electrons and Ener
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Page 2 of 2 Periodic Table Groups T
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Page 2 of 2 Using dot diagrams to r
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Page 2 of 2 13.2 Important note: If
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Page 2 of 2 Example 2: Aluminum and
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Page 2 of 2 13.2 Predict the name o
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Page 2 of 2 Using the information i
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Page 2 of 3 Conservation of atoms T
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Name: Date: 14.1 The Avogadro Numbe
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Page 3 of 4 Substance Elements in s
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Name: Date: 14.1 Formula Mass A che
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Name: Date: 14.2 Classifying Reacti
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Name: Date: 14.2 Predicting Chemica
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Name: Date: 14.2 Percent Yield You
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Name: Date: 14.4 Lise Meitner Lise
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Name: Date: 14.4 Marie and Pierre C
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Page 3 of 3 Reading reflection 1. W
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Page 2 of 2 Reading reflection 1. R
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Page 2 of 2 Reading reflection 1. U
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Page 2 of 2 1. The decay series for
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Page 2 of 2 Reading reflection 1. D
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. Page 2 of 3 i. Switches 2, 3, and
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Name: Date: 16.1 Benjamin Franklin
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Page 299 and 300: Page 3 of 4 Build a series circuit
Page 301 and 302: Name: Date: 16.3 Voltage, Current,
Page 303 and 304: Page 3 of 3 Now you will have the o
Page 305 and 306: Page 2 of 2 7. How much voltage wou
Page 307 and 308: Page 2 of 2 5. Use the series circu
Page 309 and 310: Page 2 of 2 In part (d) of problems
Page 311 and 312: Page 2 of 2 Reading reflection 1. N
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Page 317 and 318: Page 2 of 2 7. The directions—nor
Page 319 and 320: Page 2 of 2 6. Repeat step 5 to for
Page 323 and 324: Page 2 of 2 A transformer steps dow
Page 325 and 326: Page 2 of 2 4. Calculate the power
Page 329 and 330: Page 2 of 4 Determining the relativ
Page 331 and 332: Page 4 of 4 Extension—Creating cl
Page 333 and 334: Page 2 of 2 Reading reflection 1. N
Page 335 and 336: Name: Date: 19.1 Earth’s Interior
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Page 341 and 342: Page 2 of 2 Reading reflection 1. E
Page 347: Name: Date: 19.4 Continental United
Page 351 and 352: Name: Date: 20.1 Averaging The most
Page 353 and 354: Page 2 of 5 Locating the epicenter
Page 355 and 356: Page 4 of 5 20.1 For each of the pr
Page 357 and 358: Name: Date: 20.2 Volcano Parts 20.2
Page 359 and 360: Name: Date: 21.2 Calculating Concen
Page 361 and 362: Name: Date: 21.2 Solubility In this
Page 363 and 364: Page 3 of 3 The influence of temper
Page 365 and 366: Page 2 of 3 Work through these exam
Page 367 and 368: Name: Date: 21.3 Calculating pH The
Page 369 and 370: Name: Date: 22.1 Groundwater and We
Page 371 and 372: Page 3 of 3 Testing the model: 1. W
Page 373 and 374: Name: Date: 24.1 Period and Frequen
Page 375 and 376: Page 2 of 2 2. Use the grids below
Page 377 and 378: Page 2 of 2 2. Use the grids below
Page 379 and 380: Page 2 of 3 x-axis (blocks) Height
Page 381 and 382: Name: Date: 24.3 Decibel Scale The
Page 383 and 384: Page 2 of 2 a. ____________________
Page 385 and 386: Page 2 of 2 2. Two students want to
Page 387 and 388: Name: Date: 24.3 Palm Pipes Project
Page 389 and 390: Page 3 of 3 6. Challenge: You can f
Page 391 and 392: Page 2 of 2 Answer the following pr
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Page 397 and 398: Name: Date: 25.3 Using Ray Diagrams
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Page 2 of 2 2. Light strikes a mirr
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Page 2 of 2 Which way does the ligh
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Page 2 of 2 25.3 1. A lens has a fo
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Name: Date: 26.1 Gravity Problems I
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Name: Date: 26.1 Universal Gravitat
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Page 1 of 2 26.1 Nicolaus Copernicu
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Page 1 of 2 26.1 Galileo Galilei Ga
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Page 1 of 2 26.1 Johannes Kepler 26
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Name: Date: 26.1 Measuring the Moon
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Page 3 of 3 Semi-Circle Card: 26.1
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Page 2 of 2 Reading reflection 1. B
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Page 2 of 2 Part 2: Provisions for
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Page 1 of 2 27.1 Arthur Walker 27.1
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Name: Date: 27.2 The Inverse Square
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Page 2 of 3 1. Fill in the missing
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Name: Date: 28.1 Understanding Ligh
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Name: Date: 28.1 Parsecs You have a
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Page 1 of 2 28.1 Edwin Hubble Edwin
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Name: Date: 28.2 Light Intensity Pr
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Page 2 of 2 If we know the brightne
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Page 2 of 2 Solving Doppler Shift P
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13. A decimeter is 100 times larger
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Skill Sheet 1.3: Significant Digits
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7. Yes, there is a relationship bet
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6. The slope is the same (2.0) unti
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13. S Sh—Sand and shells on the b
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10. 410 miles 11. 6.6 miles -------
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Skill Sheet 4.2: Analyzing Graphs o
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Skill Sheet 5.1: Mass, Weight, and
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Skill Sheet 6.3: Applying Newton’
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Skill Sheet 7.1: Mechanical Advanta
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8. The middle gear turns left. The
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Skill Sheet 7.3: Power in Flowing E
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Skill Sheet 10.1: Calculating volum
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3. Answers are: a. 100 cm 3 b. 13 N
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Skill Sheet 11.3: Weather Maps Samp
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a. b. c. d. e f. Skill Sheet 12.2:
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Skill Sheet 14.1: Chemical Equation
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must be blocking their insulin’s
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8. The current is approximately the
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7. Students can find information ab
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Skill Sheet 17.4: Electrical Power
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Skill Sheet 19.1: Charles Richter 1
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Practice 2: 1. First problem is don
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Skill Sheet 21.3: Calculating pH 1.
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Question 8 (con’t) 9. The new wav
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Skill Sheet 25.2: The Human Eye a.
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Skill Sheet 26.1: Nicolaus Copernic
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Skill Sheet 27.1: Arthur Walker 1.
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