Total energy of particles:

Slides:



Advertisements
Similar presentations
Plate Tectonics.
Advertisements

CRCT Review SCIENCE. A student is looking at a current model of the Solar System. Which of these BEST describe the model she sees? A.) A geocentric model,
Table of Contents Section 1 The Geosphere Section 2 The Atmosphere
Chapter 2: Earth’s Structure The BIG Idea: Heat escaping from Earth’s internal layers constantly changes the planet’s surface.
Science Starter Turn to the next blank page in your ISN and cut and paste the handout that is located on the front desk. You will need colored pencils.
8 th Grade Science Final Review. Density Density is how compact something is. The formula is d = m/v As temperature increases density decreases. Less.
Created by: R. Hallett-Njuguna, SCPS Comparing Objects in Space How do the objects above compare to Earth in terms of size, distance from the Sun, and.
Heat Transfer.  Earth’s molten outer core is nearly as hot as the surface of the sun.  Heat is transferred from the core to the surface of the Earth.
Figure 1.CO2.
Matter, States of Matter, Gas Laws, Phase Changes, and Thermal Energy.
Mrs. McCarthy’s MCAS Review Earth Science 7 th Grade Curriculum –Mapping the Earth –Earth’s Structure –Heat Transfer –Earth’s History –The Earth in the.
Earth and Space Science Mrs. Jones Science Class.
Please write your name on your booklet. Please write the date of the lab test and the written test on the cover of the booklet. LAB TEST: WED. 5/20 WRITTEN.
Heat Transfer & Phases Intro Chapter. Is the ability to do work and cause a change. Can be transferred. –Gases and liquids are made of molecules that.
I can name the steps of the scientific method, in order. Structure & Transformation.
Planet Earth Getting to Know Earth The atmosphere, hydrosphere, and lithosphere form the biosphere, the part of Earth that supports life for all people,
The Dynamic Earth Chapter 3. Earth as a System  Geosphere – land 6,378 km radius  Atmosphere – mixture of gases, air  Hydrosphere – water covers 2/3’s.
Geosphere, Biosphere, Atmosphere and Hydrosphere
Density The amount of mass in a certain volume of matter.
Earth’s Internal Heat.
Unit 3 Lesson 3 Energy Transfer
Conduction, Convection and Radiation Heat Transfer.
E a r t h ’ s I n t e r i o r. The Science of Geology Geologists- scientists who study the forces that make and shape planet Earth. – They also: study.
Global average was 52.6 Class average was Living better, using less = Long, healthy lives.
Earth Science 1.2 A View of Earth. Earth’s Major Spheres  Earth is divided into 4 major spheres Hydrosphere Atmosphere Geosphere Biosphere.
The Dynamic Earth Ch. 3. Sect. 1 Objectives Describe the composition and structure of the Earth. Describe the Earth’s tectonic plates. Explain the main.
Vocabulary Click Below to start with a video – when the window opens be sure to click download.
Matter, States of Matter, Gas Laws, Phase Changes, and Thermal Energy.
Earth Astronomy 311 Professor Lee Carkner Lecture 12.
2 The Earth’s Structure series of layers or spheres which differ in density, chemistry (or composition) and physical properties.
Convection Currents and the Mantle. The Heat of the Earth Earth’s outer core is nearly as hot as the surface of the sun.
Unit 3 Lesson 2 Energy Transfer Copyright © Houghton Mifflin Harcourt Publishing Company.
Planet Earth Getting to Know Earth The atmosphere, hydrosphere, and lithosphere form the biosphere, the part of Earth that supports life for all people,
Plate Tectonics.
Unit 3 Lesson 2 Energy Transfer
Earth Systems.
Environmental Science – Chapter 3
Heat Energy.
States of Matter Matter commonly occurs in one of three “states”
I can name the steps of the scientific method, in order.
Unit 3 Lesson 2 Energy Transfer
The Earth Science Game Earth Science-1 Earth Science-2 Earth Science-3
Using Energy & Heat.
The Sun-Earth-Moon System
Plate Tectonics.
Unit 2 – Earth’s Structure
Convection and the Mantle
Convection and the Mantle
THE MOON.
Earth and Space Science
Particles in a liquid water have more energy than particles in ice.
Matter Vocabulary.
MCAS Review Earth Science By: Mrs. Edgar, Mrs. Porzio, and Ms. Robarts.
Jeopardy Ecology Geology Astronomy Energy Matter Q $100 Q $100 Q $100
CRCT 2nd Qtr. Review.
Weather dynamics Day 2 – Heat Science 10.
Matter, States of Matter, Gas Laws, Phase Changes, and Thermal Energy
Science Starter Turn to the next blank page in your ISN and cut and paste the handout that is located on the front desk. You will need colored pencils.
The Dynamic Earth.
Earth’s Interior.
Heat.
States of matter Matter- anything that has mass and takes up space.
Convection Currents and the Mantle
Convection Current.
Unit 3 Lesson 2 Energy Transfer
15.3 energy in the atmosphere
Earth and Space Science
Energy Flow in the Earth System
Changes in States of Matter
Earth Science Intro Unit
Presentation transcript:

Total energy of particles: Thermal Energy

Conservation of Energy No Energy destroyed

Movement of Thermal Energy Heat

Heat Transfer without particle movement. Conduction

Heat transfer occurs from: Hot to Cold

Addition or loss of thermal energy changes arrangement of particles during: Change of State

Temperature of Solid to Liquid Melting Point

Vaporization at Surface Evaporation

Expansion of Matter when heated: Thermal Expansion

Heated Air from Baseboard Heaters: Convection

Kinetic Energy of Particles: Temperature

Characteristic Property of Liquid: Boiling Point

How much matter an object contains? Mass

Mass in a given Volume: Density

Elements are composed of: Atoms

A group of atoms: Molecule

Substances not chemically combined: Mixture

How are liquid water, ice, and water vapor different ? Different states of matter

Distance is changing, an object is in: Motion

Speed is: Distance / Time

You know speed and direction you know: Velocity

Graphing Motion the steepness of the slope shows how: How quickly or slowly the object is moving.

Distance vs time graph a horizontal line shows: Object is not moving

300 kilometers in 3 hours you can find: Average Speed

When Speed vs Time graph is a straight line: Acceleration is constant

Model where Earth is at the center of the system of planets is: Geocentric system

The heliocentric system was supported by Galileo when he discovered: The phases of Venus

Day and night are caused by: Earth’s Rotation

Earth has seasons because: Earth’s axis is tilted as it moves around the sun.

The phase of the moon you see depends on: How much of the sunlit side of the moon faces Earth.

During a Solar Eclipse: The moon is directly between Earth and the sun.

Phase of the moon during lunar eclipse: Full Moon

Tides are caused by: Differences in how much the moon pulls on different parts of Earth.

You are less likely to see a solar eclipse than a lunar eclipse because: You must be in the moon’s shadow to see a solar eclipse.

Process that moves weathered rock: Erosion

Erosion when runoff flows in thin layer: Sheet Erosion

Wind removes surface materials: Deflation

Mechanical weathering rock is worn away by grinding of other rocks: abrasion

Earth’s Layers (From Surface) Crust, Mantle, Outer Core, Inner Core

Transfer of Energy through empty space: Radiation

Heat Transfer within a fluid: Convection Currents

The point beneath Earth’s surface where rock breaks to trigger earthquake: Focus

Risk of earthquakes on the Pacific Coast is high because: That is where the North American and Pacific plates meet.

Volcanic belts form along: The boundaries of the Earth’s plates.

The volcanoes along converging oceanic plate boundaries may form: An island arc

A volcano that may erupt in the distant future is: dormant

The place where an organism lives: Habitat

Environmental Factor that prevents a population from increasing: Limiting Factor

An organism’s role: Niche’

Study of how things interact with each other and their environment: Ecology