1. Planet Earth Chapter 1

2. Environmental Science - is the study of the infinite number of interactions between humans and the world in which we live. This includes the living and non-living factors As Earth’s human population continues to grow, as technology advances and human needs and wants increase, our impacts on the world become more widespread and severe, despite improvement in some areas.

3. 1.1 Planet of Life Living things are called organisms. Lithosphere – Layer of land that forms Earth’s surface. Hydrosphere – All the parts of Earth that are made up of water. Atmosphere – Layer of air that surrounds Earth. Biosphere – Anywhere on Earth where life exists

4. Spheres Interact Lithosphere interacts with the Hydrosphere when toxins from a factory run off into a water system and poison fish in a body of water Hydrosphere interacts with the Atmosphere when water evaporates and forms clouds Atmosphere interacts with the Lithosphere when acid rain falls and dissolves limestone

5. What’s so special about Earth? Earth supports life due to the presence of liquid water. Earth maintains a steady surface temperature due to the heat being absorbed in the summer and released in the winter through water. Many more unique qualities

6. Gas Giants Inner Terrestrial Planets

7. Planets are characterized by composition, density, and distance from the sun. The inner planets are smaller and rocky (example = Earth). The outer planets are large and made of gases (example = Jupiter). The Other 7 Planets

8. Is the sun important? Supports life on Earth by transmitting energy to us in the form of light Light travels to Earth in the form of waves

10. Why is the sky blue? A clear cloudless day-time sky is blue because molecules in the air bend blue light like a prism from the sun towards you and your eyes. At sunset, we see the red and orange colors because the light is coming at us from an angle that bends those autumn colors towards us instead of the blue.

12. 1.2 Earth’s Land and Water Lithosphere 3 Main rock types: –Sedimentary, Igneous, and Metamorphic Majority of rock is Igneous, however the rocks that we are in contact with are Sedimentary for the most part. Major Minerals – Silicates

13. Examples of Igneous rocks that would form from lava include basalt, obsidian, scoria, and pumice.

14. Rock that is changed by heat and pressure Metamorphic Rock

15. Sedimentary Rock Rock that is formed from smaller particles that are squeezed together due to pressure.

16. Hydrosphere More than 70% of Earth is covered in water. –97% of it is Salt water and 3% Fresh water

17. 2/3 or 66% of Freshwater is in our ice caps. As our ice caps melt our freshwater decreases and our saltwater increases. Surface water – ponds, lakes, and streams Groundwater - aquifers

18. What is Salt made of ? Sodium Chloride or NaCl

19. Artesian Well – Wells in which water flows to the surface due to high pressure underground. Projections have shown that natural freshwater will disappear within 40 years. Wells do not replenish as they once did due to personal demand and the amount of pavement. Aquifer – an underground layer of porous rock that contains water.

20. 1.3 The Atmosphere 4 Atmospheric layers based on temperature change. Thermosphere (Highest) Mesosphere Stratosphere Troposphere (Lowest) The atmosphere becomes less dense the farther you travel from Earth.

21. Troposphere Most weather occurs here. This is the level where we live. Closest to the Earths surface The most dense layer

22. Stratosphere Ozone Layer (Ozone – gas that blocks UV rays) Just above the Troposphere

23. Mesosphere Coldest Layer

24. Thermosphere Surprisingly the warmest layer Furthest from the surface The least dense layer

25. Facts about the Atmosphere US winds blow from the west to the east.

26. What is air composed of ? What would happen to levels of CO2 if there were fewer plants?

27. Even More Facts about the Atmosphere Ionosphere – Layer within the Thermosphere where charged particles react producing colorful displays of light called an Aurora.

29. 1.4 The Biosphere Anywhere that life can and is supported. It is 20 km thick

30. 1.4 The Biosphere Limiting Factors – things that limit life in the biosphere: Temperature Oxygen Depth Sunlight Pressure Food