Earth as a system.  Chinese (780B.C.)– earthquakes  Greeks (200B.C.) – minerals  Mayans (1100B.C.) - astronomy.

Slides:



Advertisements
Similar presentations
The Planet Oceanus. 2-1 The Earth’s Structure Earth consists of a series of concentric layers or spheres which differ in chemistry and physical properties.
Advertisements

Atmosphere, Hydrosphere, Lithosphere, and Biosphere. 5/21/2015.
Chapter 1 The Nature of Science Section 1.1 – Earth Science.
Chapter 2 Section 2 Review Page 38 Energy in the Earth System
Introduction To Physical Geology. The Science Geology is typically broken up into two fields of study –Physical Geology –Historical Geology.
Earth’s Atmosphere Part 1 - A view of Planet Earth:
Earth: The Fragile Miracle
Section 1: Earth: A Unique Planet
Earth as a System Chapter 2.
Basic Structure of the Earth
Section 1: Earth: A Unique Planet
C HAPTER 2 E ARTH AS A S YSTEM. 2.1 E ARTH : A U NIQUE P LANET Know the compositional and structural zones of Earth Explain how solar wind affect the.
Earth as a System Chapter 2.
Components of Earth.
EARTH SCIENCE – CHAP. 2 – SECT.1 OBJECTIVES 1. LIST THE CHARACTERISTICS OF EARTH’S THREE COMPOSITIONAL ZONES AND 5 STRUCTURAL ZONES 2. EXPLAIN HOW STUDIES.
Section1- Earth: A Unique Planet Section 2- Energy in the Earth System Section 3- Ecology.
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.
Earth as a System Section 1 Key Ideas Describe the size and shape of Earth. Describe the compositional and structural layers of Earth’s interior. Identify.
Earth’s Spheres & Branches of Earth Science
Views of the Earth today Earth as a system. The earth is a spherical shape It supports a complex web of life. The earth’s system has 4 major parts: –
Our Earth. Not What You Think  Earth is not a perfect sphere  Oblate Spheroid  Slightly flattened sphere  Spinning on the axis causes the polar regions.
Geosphere, Biosphere, Atmosphere and Hydrosphere
@earthscience92. What is a System? Systems – a group of interacting parts that work to together to do a job or to form a whole. Open Systems Closed Systems.
Chapter 2: Earth as a System
Ch 2-Earth as a System Objectives –Describe size and shape of Earth –Describe layers of Earth’s interior –Identify possible source of Earth’s magnetic.
STRUCTURE OF THE EARTH. Differentiation of Earth Earth is divided into layers based on density and composition Solid Layers – Core (iron-nickel) – Mantle.
Section 1: Earth: A Unique Planet
Earth Science 1.2 A View of Earth. Earth’s Major Spheres  Earth is divided into 4 major spheres Hydrosphere Atmosphere Geosphere Biosphere.
The 4 Earth Sciences. Unique Earth (The blue dot) Earth formed with the birth of our solar system, 4.6 billion years ago. –That’s 4,600,000,000 years.
The Dynamic Earth Chapter 3, sec. 1.
Earth’s Internal Structure
The Composition and Layers of the Physical Earth
Section 2: Energy in the Earth System
Chapter 2.1 Earth: a Unique Planet (Goal 1). Three Reasons the Earth is Unique … It is the only known planet with liquid surface water. It is the only.
ENVIRONMENTAL SCIENCE CHAPTER 3
© 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.
The Dynamic Earth Chapter 3. Earth consists of: Rock – geosphere Air – Atmosphere Water – hydrosphere Living things (organisms) - biosphere.
THE NATURE OF SCIENCE Earth Science is the study of the Earth Processes and Forces that change it The materials from which it is made Its long history.
Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu ES 4. Energy enters the Earth system primarily as solar radiation.
Chapter 2.1 Earth: a Unique Planet. Three Reasons the Earth is Unique … It is the only known planet with liquid surface water. It is the only known planet.
Chapter 2 - Earth as a System
Earth Basics Compositional Layers Structural Layers Ecosystems Earth’s
Why Earth Science?
The Dynamic Earth.
Earth’s Interior EQ: Describe the different layers of the earth. Explain how scientist learned about these layers.
Earth: The Fragile Miracle
Environmental Science – Chapter 3
Chapter 2 Notes Earth as a System.
Section 1: Earth: A Unique Planet
The Earth As A System.
Chapter 2.
August 25, 2017 SC. 912.E.6.1- Earth’s Layers
Chapter 2 Earth as a System 2.1 Earth: A Unique Planet
Chapter 2 Earth: A Unique Planet
Earth as a System California Standards: 4a, b; 7a, b, c
Earth’s Interior EQ: Describe the different layers of the earth. Explain how scientist learned about these layers.
Cycles Unit Two.
Spheres of the Earth.
Chapter 2 Notes Earth as a System.
Layers of the Earth Geosphere.
Chapter 2 -1 Earth: A unique planet
Chapter 1: Introducing Earth Lesson 1: Review of Earth’s System
Section 1: Earth: A Unique Planet
Properties, Systems, Interior, Exterior
Chapter 2: Earth as a System
Earth Systems: Interior of Earth
A Journey to the Center of the Earth
History of Earth.
Presentation transcript:

Earth as a system

 Chinese (780B.C.)– earthquakes  Greeks (200B.C.) – minerals  Mayans (1100B.C.) - astronomy

 Geology  Oceanography  Meteorology  Astronomy  Environmental Science

Formed about 5 billion years ago. 71% of earth is covered in ocean. Not a perfect sphere because of rotation. From space height and depth of mountains and space do not appear significant.

 Seismic activity both manmade and natural give clues to the composition of earth’s interior.  Three distinct layers  Crust  Mantle  Core

Crust – thin – accounts for 1% of the earth’s mass. – Moho (Mohorovicic) the boundary between crust and mantle layer just inside of crust. – 2 types of crust Continental – 15-80km in thickness – 2.7g/cm 3 density Oceanic – 5 to 10km in thickness. – 3.0 g/cm 3 density

 Denser material than the crust.  Thickness 2900km.  2/3 of the earth’s mass.

 Center of the earth.  Composed primarily of iron and nickel.  The iron core is about 7000km in diameter.  The outer portion being liquid and the inner portion being solid.

Composed of 5 structural zones. 1. Lithosphere – upper most part of the mantle and crust. – Solid and rigid. – 15 to 300km thick. 2. Asthenosphere – middle portion of mantle. – Solid but plastic like (plasticity). – 200 – 250 km in thickness.

3. Mesosphere – Layer below Asthenosphere more rigid is structure. 4. Outer Core – 2900km depth start the outer core believed to be liquid. 5. Inner Core – 5,150km depth starts the inner core believed to be solid.

 The earth generates a magnetic field thought to be caused by the rotation of the outer liquid iron nickel core.  This field is known as the magnetosphere and it shields the earth from cosmic radiation (solar wind).

 Atmosphere – 78% nitrogen and 21% oxygen. Upper atmosphere provides UV protection.  Hydrosphere – 71% of earth’s surface. 97% of water is salt water. The 3% that is fresh is found in lakes, streams, aquifers and ice.  Geosphere – Rock, soil, continents and oceanic floor and the molten portion of the earth.  Biosphere – The volume 8km above the earth’s surface to 8km below the earth’s surface and organic material.

 Gaia hypothesis – all organic and inorganic things work together as a system.  Two components of any system are matter and energy.  Closed System – energy can enter or exit but matter does not enter or leave.  Open System – energy and matter can leave or enter the system.

 All life at one time was believed to be dependent on energy from the sun. In the 1970’s it was found that food webs could also be dependent on chemicals ejected through deep volcanic vents found in the ocean floor.  Internal energy comes from radioactive decay and gravitational contraction.  External energy comes from the sun.

 Nitrogen cycle – used in the formation of proteins.  78% of air is Nitrogen gas.  Bacteria fix Nitrogen (make it into a useable form) for plants and then animals. NH 3, NO 3, NO 2

 Carbon forms the backbone for many organic molecules.  Carbohydrates are a primary energy source for many organisms.  Carbon dioxide can be fixed by plants into a useable form.

 Phosphorous does NOT cycle well.  Phosphorous is trapped in rocks and as weathering takes places phosphorous is released.  It is absorbed by plants and then consumed by animals.  Phosphorous is used in the formation of nucleic acids.

 Evaporation  Transpiration  Condensation  Precipitation

 Roles  Consumers  Producers  Decomposers  Carrying Capacity  Foods and Webs  Succession  Primary  Secondary

 Trophic Levels  4 to 5 levels tops  More levels at equator than at poles.  Energy Loss  Repair  Regulation  Response

 Loss of habitat  Water pollution  Greenhouse effect  Ozone Depletion  Overpopulation  …