| NYS Performance Indicators | Objectives | Text Resources | Resources (Suggested Activities) | Cross-Curriculum Connections | Assessment Items | |||
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Unit 1 - Introduction 1.1a Use standard error of measurement, and density in context |
Holt - Earth Science Chapter 1 - Section 2: Science as a Process |
“Safety Lab” “Measurement Lab” “Percent Error Lab” “Determining Density Lab” “Density of Liquids Lab” New York Science Teacher (web)When Youre Hot Youre Hot - General Lab.ds- Utilizing Probeware for the first time |
Geometry & Measurement |
EXAMGEN 4.2.3 School Island |
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Unit 2 - Astronomy 1.1a Use eccentricity, rate, gradient, standard error of measurement, and density in context |
Holt - Earth Science Chapter 27 - Section 2: Models of the Solar System |
Eccentricity Lab Using two pins and a cardboard base, students could investigate the concept of eccentricity. Students could move the pins closer together or farther apart to investigate any differences in eccentricity. Exploring the Planets CD-Rom Lab 10 Insolation-Seasons LA.doc- Utilizing probeware to determine angle of insolation |
Examgen 4.2.3 & School Island Assessment 1 Tell students they have just discovered a new planet in our solar system. Have them determine how it may have been created, the eccentricity of its orbit, period of rotation and revolution, and determine if it possesses any satellites. Upon including this information, students should also include what life would be like if they lived on that particular planet. Assessment 2 Tell students they just went back in time and everyone believes that the sun, moon and planets move around Earth. Their job is to convince the public that this belief is not true. They are to present as many forms of evidence as possible. |
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2.1b Understand the relationships among: the planets' distance from the Sun, gravitational force, period of revolution, and speed of revolution |
Holt - Earth Science Chapter 27 - Section 2: Models of the Solar System |
See above | See above | ||||
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1.1a Show how our observation of celestial motions supports the idea of stars moving around a stationary Earth (the geocentric model), but further investigation has led scientists to understand that most of these changes are a result of Earth's motion around the Sun (the heliocentric model) |
Holt - Earth Science Chapter 27 - Section 2: Models of the Solar System |
Discussion Activity As long ago as 350 B.C., Aristotle proposed searching for stellar parallax to resolve the heliocentric/geocentric controversy. Trace the history of this search through Tyco Brahe (1600), William Herschel (1770), and Friedrich Bessel (1840). What were some of the explanations considered for the failure to find stellar parallax for such a long time. |
Armageddon Internet Project | ||||
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3.1a Determine the changing length of a shadow based on the motion of the Sun |
Holt - Earth Science Chapter 26 - Section 2: Movements of Earth |
See above | See above | ||||
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1.1a Most objects in the solar system are in regular and predictable motion.
1.1e The Foucault pendulum and the Coriolis effect provide evidence of Earth's rotation. 1.1f Earth's changing position with regard to the Sun and the moon has noticeable effects.
1.1h The Sun's apparent path through the sky varies with latitude and season. 1.1i Approximately 70 percent of Earth's surface is covered by a relatively thin layer of water, which responds to the gravitational attraction of the moon and the Sun with a daily cycle of high and low tides. |
Holt - Earth Science Chapter 26 - Section 2: Movements of EarthHolt - Earth Science Chapter 28 - Section 2: Movements of the Moon |
Exploring the Planets CD-Rom Lab The Suns Path Lab The Use of a Foucault Penulum Lab Classroom Activity Attach names of four different constellations to the four walls of room. Clear out center of room so that students can assemble in a large circle. Place a lamp in the center to simulate the sun. Have students form circle facing the “sun”. Ask students to imagine that a little person is standing on the end of their nose looking down at their feet. Ask students “what time is it for the little person”? (Correct response is that it is noon for the little person as the sun is directly overhead.) Now ask them to make it midnight for the little person. (Students should rotate, counterclockwise 180 degrees) Now that they are facing away from the sun, ask them to notice the constellation they are looking at. Ask students to make it noon again. Ask them how much time has gone by? Ask what motion 1 day is based on? Now ask students to make 6 months go by. (Students will eventually “revolve” halfway around the sun) Ask students to describe one year. Have students make it midnight for the little person an ask them to notice what constellation is visible. Ask them why it is not the same as 6 months ago. Ask them if they think that constellations visible in the summer will be visible in winter. Ask them to explain why. You may want to discuss circumpolar constellations such as Polaris. Eclipses Interactivity (WEB) |
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1.2a The universe is vast and estimated to be over ten billion years old. The current theory is that the universe was created from an explosion called the Big Bang. Evidence for this theory includes:
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Holt - Earth Science Chapter 30 - Section 1: Characteristics of Stars Chapter 30 - Section 2: Stellar Evolution Chapter 30 - Section 3: Star Groups Chapter 30 - Section 4: The Big Bang Theory |
Various Astrological Observations | |||||
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1.2c Our solar system formed about five billion years ago from a giant cloud of gas and debris. Gravity caused Earth and the other planets to become layered according to density differences in their materials.
1.2f Earth's oceans formed as a result of precipitation over millions of years. The presence of an early ocean is indicated by sedimentary rocks of marine origin, dating back about four billion years. |
Holt - Earth Science Chapter 27 - Section 1: Formation of the Solar System Chapter 27 - Section 3: The Inner Planets Chapter 27 - Section 4: The Outer Planets |
Create a Scaled-Down Version of the Solar System | |||||
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3.1a Develop a scale model to represent planet size and/or distance |
Holt - Earth Science Chapter 27 - All Sections |
Create a Scaled-Down Version of the Solar System |
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Unit 3 - Dimensions of the Earth 1.1a Use of gradient formula. |
Holt - Earth Science Chapter 3: Models of the Earth |
Gradient Lab Using Contour Map Same technology links as above25 Mapping LA.doc- Probeware lab |
Examgen 4.2.3 & School Island Assessment: Tell students they have just landed on a previously undiscovered planet in our solar system and their job is to determine it shape and size and then to map the surface features that are found there. Give students photos of the night sky supposedly taken from the planet, charts that show the angle and path of the sun at different locations on the planet, descriptions of the behavior of objects as they appear and disappear on the horizon, etc. Have different information sets so that students have planets of varying sizes and shapes. Once size and shape have been determined, give students plastic models, which show exhibit various topographic features (these might be obtained from local geologic society or university). Students must create a topographic map of their model which accurately depict the distances, elevations, and shapes of their region. |
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3.1a In a field, use isolines to determine a source of pollution |
Holt - Earth Science Chapter 1 - Section 3: Models of the Earth |
See above | See above | ||||
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3.1a Determine the changing length of a shadow based on the motion of the Sun |
Holt - Earth Science Chapter 29 - The Sun |
Flashlight Demonstration | |||||
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2.1q Topographic maps represent landforms through the use of contour lines that are isolines connecting points of equal elevation. Gradients and profiles can be determined from changes in elevation over a given distance. |
Holt - Earth Science Chapter 3: Models of the Earth |
Using Topographic Maps Lab Creating Topographic Maps Reading Topographic Maps Lab Journey Home Lab Contour Plates Lab Where is the Stanley Cup? Lab |
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1.1c Earth's coordinate system of latitude and longitude, with the equator and prime meridian as reference lines, is based upon Earth's rotation and our observation of the Sun and stars. |
Holt - Earth Science Chapter 3: Models of the Earth |
See above | |||||
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2.2a Draw a simple contour map of a model landform 2.2b Design a 3-D landscape model from a contour map 2.2c Construct and interpret a profile based on an isoline map |
Holt - Earth Science |
Topographic Profiles Lab Using Topographic Maps Lab Creating Topographic Maps Reading Topographic Maps Lab Journey Home Lab |
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3.1c Use topographical maps to determine distances and elevations |
Holt - Earth Science Chapter 3: Models of the Earth |
See above | |||||
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2.1b Using a topographic map, determine the safest and most efficient route for rescue purposes |
Holt - Earth Science Chapter 3: Models of the Earth |
See above | |||||
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Earth Science Planning for Results (2010-11).pdf |