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What qualities are present at divergent boundaries? (1)

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1

What qualities are present at divergent boundaries? (1)

  • small shallow earthquakes on boundaries

  • not many volcanoes

  • crust slightly shallower along plate boundary

  • symmetrical age — newer at boundary, gets older further away

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2

What qualities are present at convergent boundaries? (1)

  • Earthquakes get shallower on side going under, get deeper as earth descends

  • Volcanoes along top plate parallel to boundary

  • Volcanic arc next to deep sea trench

  • Likely no symmetry, geochronology not related to convergent boundary

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3

What qualities are present at transform boundaries? (1)

  • Lots of shallow earthquakes along the boundary

  • No volcanoes forming

  • Off-set streams, physical cracks on landscape

  • No formation or recycling of crust

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4

What rocks were present at Vasquez Rocks and what was the sorting like?

  • Quartz, k-feldspar and amphibole were present

  • Rocks were sedimentary

  • Poor sorting — rocks vary greatly in size and indications of flash floods (high energy)

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5

What rocks were present at Devil’s Punchbowl?

  • Sedimentary

  • Granite, andesite, biotite, k-feldspar, quarts, sandstone, gneiss, diorite

  • There is less variety than there used to be in ancient times

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6

What type of rock is best to build on for earthquakes?

Sandstone is best, unstable river gravel and artificial fill are the worst

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7

How do igneous rocks form and what do the different grain size/texture mean about the cooling rate?

  • Form when molten rock cools and becomes solid

  • Cool slowly —> larger minearls (macrocrystalline)

  • Cool quickly —> smaller minerals (microcrystalline)

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8

What is the difference between intrusive, extrusive, and porphyritic rocks?

  • Intrusive - tend to be macrocrystalline (cool inside Earth)

  • Extrusive - microcrystalline (cool outside Earth)

  • Porphyritic - microcrystalline with scattered large crystals

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9

What are the seven main igneous rocks and what are they made of?

  • Granite (k-feldspar, biotite, quartz)

  • Basalt (pyroxene)

  • Diorite (plagioclase feldspar, amphibole)

  • Gabbro (pyroxene, plagioclase feldspar)

  • Peridotite (olivine)

  • Porphyritic andesite (amphibole)

  • Porphyritic rhyolite (quartz, muscovite, amphibole)

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10

What is the difference between detrial, organic and inorganic sedimentary rocks and how they form?

  • Detrial — made of fragments of pre-existing rocks that have been broken down through weathering erosion (mudtsone, shale, sandstone, breccia and conglomerate)

  • Organic — made of organic material produced by fossils (calcite)

  • Inorganic — formed from sediment that precipitates water — only chemical sediment (rock salt and gypsum)

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11

What causes foliated vs non-foliated metamorphic rocks?

  • Foliated — form as a result of regional metamorphism (usually directed pressure); greater degree of metamorphism → larger minerals; more metamprophism = more shiny

  • Non-foliated — macroscopic tecture, high temp WITHOUT direct pressure, likely consist of one mineral

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12

What is an epicenter vs a focal point?

  • Epicenter — point on Earth’s sruface above focal point

  • Focal point — underground origin of the earthquake

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13

How do earthquakes occur?

  • Plate tectonic motion builds up as strain within Earth taht releases along faults

  • Seismic waves originate at focal point and travel in all directions

  • Motion (slip) along fault is what people feel

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14

What is the stike vs the dip?

  • Strike — line of intersection btwn inclinced plane of sedimentary bed and horizontal plane

  • Dip — maximum tilt angle of sedimentary bed

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15

What types of rocks on are Fiji Hill and when did they form?

  • Topanga formation — sedimentary rock

  • Formed 13 million years ago (young)

  • Granite, quartz, k-feldspar, plagioclaste, biotite

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16

What types of clasts are present and how did the rocks move from the San Gabriel mountains?

  • Moved as the mountain eroded through landslides and then moved by streams/erosion to where they are

  • Fragments are buried and then lithification occurs → uplift happens

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17

What is the geologic history of the Topanga formation?

  • Crystallization of intrusive rocks

  • Uplift

  • Erosion

  • Sedimentation

  • Litification

  • Uplift

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18

At what rate is Fiji eroding?

.12 inches/year —> 100 feet will be eroded in 10,000 years

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19

What are the features of Mt Waddington, BC that indicate it formed from a glacier?

U-shape channel

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20

What direction was the Rhone Glacier moving and what direction was the terminus moving?

East because stakes are displaced to the East, northwest

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21

How fast was the average rate of flow (in meters/year) in the center and near the edge?

16 m/year in the center and 75 m/year at the edge (flowed faster at the edge)

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22

What was the average rate of retreat of the Rhone glacier?

20 m/year

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23

What order were glaciers forming Bloody Canyon, Sawmill and Grant Lake?

Bloody Canyon — Tenaya (mid)

Sawmill — Tahoe (oldest)

Grant Lake — Tioga (youngest)

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24

What phyla and class are corals part of?

Phylum Cnidaria

Class Anthozoa

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25

What phyla are fan, corkscrew and twig like shapes part of?

Phylum bryozoa

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26

What phylum are small, shell organisms apart of?

Phylum brachiopoda

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27

What phylum and class are clams, oysters and mussels part of?

Phylum mollusca

Class bivalvia

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28

What phyla and class are snails a part of?

Phylum mollusca

Class gastropoda

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29

What phyla and class are animals like squids?

Phylum mollusca

Class cephalopoda

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30

What phyla and class are three-lobed scavengers part of?

Phylum arthropoda

class trilobita

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31

What phyla and class are sea lilies?

Phylum echinodermata

Class crinoidea

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32

What phyla and class are sea urchins and sand dollars?

Phylum echinodermata

Class echinoidea

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