1 / 17

Bellwork 1/31

Bellwork 1/31. The earliest land plants did not have flowers. However, around 70 million years ago, flowering plants became the dominant plant type in many habitats. Which type of organism would benefit directly from the increase in flowering plants?

edna
Télécharger la présentation

Bellwork 1/31

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Bellwork 1/31 The earliest land plants did not have flowers. However, around 70 million years ago, flowering plants became the dominant plant type in many habitats. Which type of organism would benefit directly from the increase in flowering plants? A. Aquatic mammals, which are able to use the plants for shelter B. Anaerobic bacteria, which can thrive in low oxygen environments C. Pollinating insects, which consume nectar and pollen as food sources D. Carnivorous reptiles, which are able to hunt for food among the plants

  2. Bellwork 2/1 The following chemical equation shows the incomplete formula for burning methanol. The question mark represents the unknown number of oxygen (O2) molecules. 2CH3OH +?O22CO2+4H2O How many molecules of O2 are needed to balance this chemical equation? F. 1 G. 3 H. 5 J. 6 TURN IN BELLWORK WHEN YOU ARE FINISHED!!!!

  3. Plate tectonics The movement of Earth

  4. Continental Drift • The continental drift hypothesis – continents have moved slowly to their current locations • All continents were once connected as one large landmass now called Pangaea • The land mass broke apart, and the continents drifted to their present positions • Evidence for continental drift • Puzzle-like fit of the continents • Similar fossils have been found on different continents • Remains of warm weather plants in Arctic areas and glacial deposits in tropical areas suggest that continents have been moved • Similar rock structures are found on different continents

  5. Continental Drift • At first, continental drift was not accepted because no one could explain how or why continents had moved.

  6. Discussion Question • Why is the fact that similar fossils have been found on different continents considered evidence for continental drift? • If fossils of similar plants and animals are found on widely separated continents, it is more likely that the continents had once been joined than that the plants and animals migrated.

  7. Seafloor Spreading • Using sound waves, scientists discovered a system of underwater mountain ranges called the mid-ocean ridges in many oceans. • In the 1960s, Harry Hess suggested the theory of seafloor spreading to explain the ridges • Hot, less dense material below Earth’s crust rises upward to the surface at the mid-ocean ridges. • Then, it flows sideways, carrying the seafloor away from the ridge • As the seafloor spreads apart, magma moves up and flows from the cracks, cools, and forms new seafloor

  8. Seafloor Spreading • Evidence for seafloor spreading • Youngest rocks are located at the mid-ocean ridges • Reversals of Earth’s magnetic field are recorded by rocks in strops parallel to ridges

  9. Discussion Question • How could seafloor spreading be related to continental drift? • If the seafloor is constantly spreading apart and moving, it will affect and move the continents as well.

  10. Theory of Plate Tectonics • Plate movements • Earth’s crust and upper mantle are broken into sections • The sections, called plates, move on a plastic-like layer of the mantle • The plates and upper mantle form the lithosphere • The plastic-like layer below the lithosphere is called the asthenosphere

  11. Theory of Plate Tectonics • Plate boundaries • Plates moving apart – divergent boundaries • Plates moving together – convergent boundaries • Denser plates sink under less dense plates • Newly formed hot magma forced upward forms volcanic mountains

  12. Theory of Plate Tectonics • Plates collide • Plates crumple up to form mountain ranges • Earthquakes are common

  13. Theory of Plate Tectonics • Plates slide past – called transform boundaries; sudden movement can cause earthquakes

  14. Theory of Plate Tectonics • Convection inside Earth – the cycle of heating, rising, cooling, and sinking of material inside Earth is thought to be the force behind plate tectonics • Features caused by plate tectonics • Faults and rift valleys • Mountains and volcanoes • Strike-slip faults – cause of earthquakes • Testing for plate tectonics – scientists can measure movements as little as I cm per year

  15. Theory of Plate Tectonics

  16. Theory of Plate Tectonics

  17. Discussion Question • What will happen if a continental plate collides with an oceanic plate? • A continental plate with a continental plate? • Why? • The denser plate will always subduct, or bend under, the less dense plate. Oceanic plates are denser than continental plates, so the oceanic plate will sink under it. When two continental plates collide, neither will subduct because they are both less dense than the asthenosphere beneath them. Instead, they will crumple up and form mountain ranges

More Related