NOTES: Earth: Age--4.6 billion years by radioactive isotope dating.

Slides:



Advertisements
Similar presentations
Angstrom Care 培苗社 Rocks II
Advertisements

Rocks and Fossil Fuels.
The Living Earth Chapter Nine.
Weather & Climate.
Rocks Here, There, Everywhere
Integrated Science One
EARTH’S ATMOSPHERE Chapter 14.1 Pages
WEATHER AND CLIMATE. ATMOSPHERE The atmosphere is a collection of gases that makes the Earth habitable.
Stratosphere Troposphere
Air Pressure and Wind Chapter 10 Lesson 6.
Riddles What happens when you throw a yellow rock into a purple stream? What starts with a T, ends with a T, and has T in it?
Crustal Movement.
Chapter 17 Notes: The Atmosphere. What is the Atmosphere? The atmosphere can be defined as the portion of planet earth that contains gas. Weather can.
Sponge: List the six layers of the Earth.. Atmosphere A mixture of gases: N 2 78% O 2 21% Ar0.9% CO %
Earth’s Atmosphere. What newsworthy weather events have you noticed in the media?
1. angular resolution ability to distinguish between two adjacent objects in the sky.
Earth as a System Chapter 2.
Earth as a system.  Chinese (780B.C.)– earthquakes  Greeks (200B.C.) – minerals  Mayans (1100B.C.) - astronomy.
Earth’s Atmosphere.  The three main features of the Earth are the land, the water and the air.  Land areas include the seven continents and other landmasses.
The Earth and Its Moon The Earth Solid inner core, liquid outer core atmosphere - 50km thick magnetosphere - charged particles caught in Earth’s magnetic.
Structure of the Earth Geology 12 Ms. Pushie CHS
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.
Atmosphere and Weather AP Environmental Science.
Geosphere, Biosphere, Atmosphere and Hydrosphere
Rocks.
Earth’s Atmosphere The Earth is surrounded by a blanket of air called the atmosphere. It extends over 372 miles (560 kilometers) from the surface of Earth.
The surrounding air of the Earth
By Gabriel Anurum Earth Earth is a complex place, usually to understand complex things people break them down to understand it. Scientist divide earth.
Earth Formation and Structure. Early Earth: Age and Formation Condensed from solar nebula 4.6 billion years ago along with the rest of the planets in.
UNIT 1: EARTH SYSTEMS Environmental Science. Connection The Earth as a System: The Earth consists of rock, air, water, and living things that all interact.
Know about the Earth’s Interior Know about the Earth’s Atmosphere Know about the Earth’s Magnetic Field The Earth – Inside and Out.
Preview Section 1 Characteristics of the Atmosphere
Have you ever wondered how a compass works? Compasses How many of you have used a compass before? Can you explain how it works?
Planet Earth What would alien astronomers observe? Chapter 4 Page
ISP Astronomy Gary D. Westfall1Lecture 9 Earth as Planet The Earth is a medium size planet with a diameter of 12,756 kilometers (7926 miles) Composed.
Chapter 5 Earth and its Moon. The Earth Table 5-1 Some Properties of Earth and the Moon.
Chapter 7 Earth. Mantle Two-part core Thin crust Hydrosphere (oceans) Atmosphere Magnetosphere Structure of Planet Earth.
Forces that act on the Earth. The Inner Core The deepest layer in Earth is the inner core. It is located at the center of Earth because it contains.
1. What do we call the thin layer of gasses that surround the earth? Atmosphere.
By: Baylee.  We have been studying the Earth and rock cycle in class. Most of what we have learned has come from our readings and class discussion, as.
Science 8 th Grade Geology Part 3 Rocks Standard A.
Chapter 8 The Earth. How do we know that planet Earth really revolves and rotates? What is Aberration and what does it prove about the Earth? What is.
© 2009 W.W. Norton Earth Liquid water on its surface Oxygen atmosphere Only planet known to support life 4.6 billion years old 71% covered by H 2 O Oblate.
There are 4 main layers that make up the earth: The crust The mantle The outer core The inner core.
Earth Earth is the third planet from the sun. It has volcanoes like on Venus and Mars, craters like those found on Mercury, and swirling weather systems.
Three Types of Rock.
© Sierra College Astronomy Department Terrestrial Geology Basics.
Unit 2: The Dynamic Earth Mr. Ross Brown Brooklyn School for Law and Technology.
Earth’s Layers Geology Unit.
THE ROCK CYCLE.
Alta High Astronomy Chapter 7 Earth: Our Home in Space.
Ocean Water.
Sponge: List the six layers of the Earth.
Ocean Water.
Layers, Temperature, Pressure, Wind, Coriolis Effect
Daily Starter When you get your composition books.
The Atmosphere.
Earth as a Magnet.
Layers of the Atmosphere
Chapter 15: Atmosphere.
Virtual Rock Collection
Do Now: What is your favorite layered food?
WEATHER AND CLIMATE.
Spheres of The Earth.
Chapter 1: Introducing Earth Lesson 1: Review of Earth’s System
Three Types of Rock.
Earths Atmosphere.
CLASSIFICATION IS IT A ROCK OR A MINERAL? BECOME A ROCK HOUND.
Earth How We Know What We Know The Inside Volcanoes The Outside Drills
Chapter 5 Ecosystems and the Physical Environment
Presentation transcript:

NOTES: Earth: Age--4.6 billion years by radioactive isotope dating. Atmosphere--80% Nitrogen, 20% Oxygen, trace of Carbon Dioxide. Pressure = 14.7 lbs/sq in. Originally lots of CO2, but oceans absorbed it, plankton and plant life converted it to O2. Troposphere--0-10 km--weather here. Planes must go above. Stratosphere--11-50 km--ozone layer (helped life move to land) Mesosphere--50-90 km --temperature decrease Ionosphere--above 90 km--aurora generated here--temp. rises History--earth was once molten, radioactivity provided heat to keep the core molten, substances segregated. We know core is denser iron and nickel because density of earth = 5.5 g/cm3, but surface rocks have a lower density than that. Layers of the earth: (see overlay) In addition part of the mantle and the whole crust make up the lithosphere, the rolling crustal plates. Wegener's theory of continental drift. (See map.) Magnetosphere: the realm of the earth's magnetic field extending into space. Electrons in the solar wind are trapped in the Van Allen Belts (overlay). Aurora (northern and southern lights) caused by electrons in solar wind whirling around magnetic field lines and radiating. Weather: earth's rotation yields Coriolis force--winds counter- clockwise in northern hemisphere, clockwise in southern.

Age (from oldest rocks): 4.6 Billion Years

Atmospheric Layers

History--earth was once molten, radioactivity provided heat to keep the core molten, substances segregated, heavier ones drawn to center by gravity. Earth’s core is mostly iron and nickel.

Layers of the Earth How do we know? Seismology—earthquake waves. We also know core is denser iron and nickel because density of earth = 5.5 g/cm3, but surface rocks have a lower density than that.

A lesson in Geology that really ROCKS! Three major types of rock.

Igneous rocks form when molten rock cools and becomes solid. Molten rock is called magma when it is below the Earth’s surface and lava when it is above.

Sedimentary rock For thousands, even millions of years, little pieces of our earth have been eroded--broken down and worn away by wind and water. These little bits of our earth are washed downstream where they settle to the bottom of the rivers, lakes, and oceans. Layer after layer of eroded earth is deposited on top of each. These layers are pressed down more and more through time, until the bottom layers slowly turn into rock.

Metamorphic rocks are rocks that have "morphed" into another kind of rock. These rocks were once igneous or sedimentary rocks. How do sedimentary and igneous rocks change? The rocks are under tons and tons of pressure, which fosters heat build up, and this causes them to change. If you examine metamorphic rock samples closely, you'll discover how flattened some of the grains in the rock are.

Part of the mantle and the crust make up the lithosphere, the rolling crustal plates.

In about 1911, Alfred Wegener learned a dance called the Continental Drift  Heat makes lower mantle flow in circular patterns, Breaking up lithosphere and moving the continents.

Modern reconstruction of Pangaea, ca. 255 million years ago

Compass points in direction of magnetic field lines. The north magnetic pole really is in the north (not south).

Aurora: northern and southern lights-- Aurora Borealis and Australialis Caused by solar wind hitting earth’s magnetic field.

Auroras result from emissions of photons in the Earth's upper atmosphere, above 80 km (50 miles), from ionized nitrogen atoms regaining an electron, and oxygen and nitrogen atoms returning from an excited state to ground state. They are ionized or excited by the collision of solar wind particles being funneled down and accelerated along the Earth's magnetic field lines; excitation energy is lost by the emission of a photon of light, or by collision with another atom or molecule: oxygen emissions Green or brownish-red, depending on the amount of energy absorbed. nitrogen emissions Blue or red. Blue if the atom regains an electron after it has been ionized. Red if returning to ground state from an excited state. From Wikipedia on ‘Aurora (Astronomy)’

Composed of electrons ‘boiling’ off the sun.

The Van Allen Belts: trapped charged particles between magnetic field lines. A third belt has been found.

Gaspard-Gustave de Coriolis An engineer and physicist, He introduced the terms 'work' and 'kinetic energy' with their present scientific meaning, and studied flow on a rotating body like the Earth.

The Coriolis effect causes wind flowing from high pressure to low pressure regions to curve as the wind moves. This creates the trade winds. In the Northern Hemisphere, the Coriolis effect causes flow to curve to the Right In the Southern Hemisphere, the Coriolis effect causes flow to curve to the Left