1 / 20

Bowen’s Reaction Series

Bowen’s Reaction Series. basaltic magma rhyolitic/granitic magma igneous rocks basaltic lava andesitic lava diorite intrusive rocks scoria. andesitic magma gabbro rhyoliotic/granitic lava andesite extrusive rocks pumice pegmatite.

Download Presentation

Bowen’s Reaction Series

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. Bowen’s Reaction Series

  2. basaltic magma rhyolitic/granitic magma igneous rocks basaltic lava andesitic lava diorite intrusive rocks scoria andesitic magma gabbro rhyoliotic/granitic lava andesite extrusive rocks pumice pegmatite Construct a concept map using the following terms:

  3. Use the sedimentary identification table to name this rock.

  4. Long profile of a typical stream

  5. Stream channel near the headwaters (start of a stream)

  6. Long profile of a typical stream

  7. Stream channel near the middle of a typical stream profile

  8. Long profile of a typical stream

  9. Stream channel near the mouth (end) of a stream Link 1 Link 2

  10. Stream Velocity VS. Sediment Size • A streams velocity is 100 cm/sec. List the sediments that will be carried by the stream. • A streams velocity is 40 cm/sec. List the sediments that will be carried by the stream. • State the relationship between stream velocity and particle size. • Describe how the size and shape of most pebbles change when the pebbles are transported in a stream over a great distance.

More Related