Rocks for Astronomers Astronomy...

8
1 Slide 1 Geology of Puerto Rico An Overview of the Plate Tectonic Origin of the Caribbean Slide 2 Outline Rock types in Puerto Rico Plate Tectonics review Puerto Rico formed WHERE? • Evidence Tectonic Reconstruction Slide 3 Rocks for Astronomers Astronomy: H,He Metals Geology: Basalt Other Puerto Rico Volcanic Marine Olivine Limestone Mg 2 SiO 4 CaCO 3 Slide 4 Astronomy (simplified) • Hydrogen • Helium Metals (everything else) Slide 5 Astronomy Geology Rocks • Hydrogen • Helium • Metal (everything else) Hot (igneous) • Medium (metamorphic) Cold (sedimentary) Slide 6 Geology (continued) Hot = Igneous - Volcanic rocks, basalt Lava is molten on the surface, cools quickly Granite is molten underground, cools slowly Medium = metamorphic Re-heating of rocks, re-crystalization Cooking of limestone makes marble Cold = sedimentary Carried by wind or water, like sandstone Layered sands from dunes near the shore ( look along the Jobos beach road cut)

Transcript of Rocks for Astronomers Astronomy...

Page 1: Rocks for Astronomers Astronomy (simplified)naic.edu/~astro/School/Talks/howell_geology.pdf“plates” (lithosphere) • The plates move on top of a plastic layer of rock (aesthenosphere)

1

Slide 1

Geology of Puerto RicoAn Overview of the Plate Tectonic

Origin of the Caribbean

Slide 2

Outline

• Rock types in Puerto Rico

• Plate Tectonics review

• Puerto Rico formed WHERE?

• Evidence

• Tectonic Reconstruction

Slide 3

Rocks for Astronomers

Astronomy: H,He Metals

Geology: Basalt Other

Puerto Rico Volcanic Marine

Olivine Limestone

Mg2SiO4 CaCO3

Slide 4

Astronomy (simplified)

• Hydrogen

• Helium

• Metals (everything else)

Slide 5

Astronomy Geology Rocks

• Hydrogen

• Helium

• Metal

(everything else)

• Hot (igneous)

• Medium (metamorphic)

• Cold (sedimentary)

Slide 6

Geology (continued)

• Hot = Igneous - Volcanic rocks, basalt– Lava is molten on the surface, cools quickly– Granite is molten underground, cools slowly

• Medium = metamorphic– Re-heating of rocks, re-crystalization– Cooking of limestone makes marble

• Cold = sedimentary– Carried by wind or water, like sandstone– Layered sands from dunes near the shore ( look along

the Jobos beach road cut)

Page 2: Rocks for Astronomers Astronomy (simplified)naic.edu/~astro/School/Talks/howell_geology.pdf“plates” (lithosphere) • The plates move on top of a plastic layer of rock (aesthenosphere)

2

Slide 7

Basalt flow in Hawaii

Slide 8

Puerto Rico Geologic Map

Slide 9

Puerto Rico Geologic Regions

Slide 10

Puerto Rico faults and intrusions

Slide 11

Geology Field Trip

• Let’s look at a nearby outcrop of limestone

• (How often have you had an astronomy field trip?)

Slide 12

Limestone Fossils

Page 3: Rocks for Astronomers Astronomy (simplified)naic.edu/~astro/School/Talks/howell_geology.pdf“plates” (lithosphere) • The plates move on top of a plastic layer of rock (aesthenosphere)

3

Slide 13

More Fossils

Slide 14

Structure of the Earth

• Earthquakes tell us about the interior structure

• Earthquakes generate P-waves and S-waves• P-waves are pressure waves – in direction

of motion• S-waves are shear waves – perpendicular to

the direction of motion • S-waves do not propagate through liquids

Slide 15 Fig. 6-7, p.101 Slide 16

Seismology:a way to probe the Earth’s interior

Slide 17

Global Tectonic Plates and Earthquakes

Slide 18

Plate Tectonics Overview

• Earth surface is made up of semi-rigid “plates” (lithosphere)

• The plates move on top of a plastic layer of rock (aesthenosphere)

• The driving force is convection in the mantle

• Heat from the core fuels the system

Page 4: Rocks for Astronomers Astronomy (simplified)naic.edu/~astro/School/Talks/howell_geology.pdf“plates” (lithosphere) • The plates move on top of a plastic layer of rock (aesthenosphere)

4

Slide 19 Fig. 6-3, p.98 Slide 20

Types of Plate Boundaries

• Divergent – Spreading ridge (Atlantic)

• Convergent – Subduction Zone (Lesser Antilles, Pacific Rim)

• Neither - Transverse fault (San Andreas Fault, Puerto Rican trench at present)

Slide 21

Global Tectonic Plates

Slide 22

Island Arc formation at a Subduction Zone

Slide 23

Monserrat VolcanoSoufriére Hills

Slide 24

Before After

Page 5: Rocks for Astronomers Astronomy (simplified)naic.edu/~astro/School/Talks/howell_geology.pdf“plates” (lithosphere) • The plates move on top of a plastic layer of rock (aesthenosphere)

5

Slide 25

Subduction of a spreading center

•Subduction cut off

•New trench forms on the other side

•Same volcanos may be activated

Slide 26

Slide 27

Caribbean Plate Todayboundary and geologic regions

Slide 28

Tectonic Setting

Slide 29 Slide 30

Plate Tectonic Reconstruction of the Caribbean region:

200 million years ago to present

Page 6: Rocks for Astronomers Astronomy (simplified)naic.edu/~astro/School/Talks/howell_geology.pdf“plates” (lithosphere) • The plates move on top of a plastic layer of rock (aesthenosphere)

6

Slide 31 Slide 32

Slide 33 Slide 34

Slide 35 Slide 36

Page 7: Rocks for Astronomers Astronomy (simplified)naic.edu/~astro/School/Talks/howell_geology.pdf“plates” (lithosphere) • The plates move on top of a plastic layer of rock (aesthenosphere)

7

Slide 37 Slide 38

Slide 39 Slide 40

Slide 41 Slide 42

Page 8: Rocks for Astronomers Astronomy (simplified)naic.edu/~astro/School/Talks/howell_geology.pdf“plates” (lithosphere) • The plates move on top of a plastic layer of rock (aesthenosphere)

8

Slide 43 Slide 44

Slide 45

Caribbean Plate Todayboundary and geologic regions

Slide 46

Puerto Rico and Virgin Islands microplate