Photo Review  

This page is always under construction. 
If you find a photo, diagram or video you think should be included 
please send a copy or link to mvosguenter@sd62.bc.ca 

TERM 3

Introduction

Introduction to Geology (Chapter 1) 

Surface Processes and the Hydrosphere 

Surface Processes I

Weathering and Erosion (Chapters 5, 18 + 19)

Surface Processes II

Running Water (Chapter 14)
Ground Water (Chapter 15)

Surface Processes III

Glaciers (Chapter 17)

Comparative Planetology
Inner and Outer Planets (Chapter 22)

Earth Resources

Mineral & Energy Resources (Chapters 20+21)

Earth Materials (Rocks and Minerals)

Minerals (Chapter 2) 


TERM 4

Volcanoes (Chapter 4)

Igneous Rocks and Processes (Chapter 3) 

Sedimentary Rocks (Chapter 6) 

Metamorphic Rocks (Chapter 7)

Geologic Time

Relative Dating (Chapter 8) 
Absolute Dating
(Chapter 8) 
Geologic Time Scale
(Chapter 8) 
The Fossil Record  (lab activities)
  

Internal Processes and Plate Tectonics

Plate Tectonics (Chapter 9) 

accretionary wedge
Benioff Zone
continental drift
convergent boundaries
convection cell
crust
divergent boundary

Hawaiian Islands
hotspot (1) hotspot (2)
plate boundaries - map
polarity reversal
    /
Juan de Fuca Ridge
ridges and rises
ridge push

sea floor spreading
slab pull
subduction 
terrane / NA Terranes
transform boundary 
   /
fracture zone

trench

Earthquakes (Chapter 10)

dilatancy
deep-focus
earthquake 
elastic rebound
epicentre vs focus

fault creep / example
liquefaction / example
shear force / example
seismic waves

seismic gap

seismogram
seismogram - types
seismograph
tsunami

Earth's Interior (Chapter 11) 

Earth's interior (1)

Earth's interior (2)

Shadow Zone

Active Margin Passive Margin Seismic Evidence

Isostasy (Chapter 12)  

Isostasy is the vertical movement of the crust in response to buoyancy in the mantle. Variations in elevation are due both to thickness and density of the crust. 

isostasy1.jpg (40697 bytes) 
What will happen to the springs
 when she gets up?

 isostasy.jpg (42044 bytes) 
or to the crust 
when the ice melts?

Shorelines have nothing to do with the boundary between continental granitic crust and oceanic basaltic crust.

isostacy-Rhossili-RaisedBeach.jpg (76435 bytes)
 
 Isostatic Rebound...
= Raised Beach

isostacy-hysevm.jpg (44634 bytes) 
Isostatically-raised beaches near Pointe aux Chenes, Lake Michigan


 
Just like blocks of wood in water float higher the thicker they are, the crust rises and sinks because it is lighter than the underlying mantle.

 
The continents stand high because continental crust is thick and light. The ocean basins are low because oceanic crust is thin and dense.

 

Structural Geology (Chapter 12)

anticline

basin

block diagram

compressional force

cross section

dip

dip-slip

directed stress 

dome

fault

fold

geological map

joint

normal fault

overturned fold

recumbent fold

reverse fault

shear force

strike

strike-slip

syncline

tensional force

thrust fault

transform

unconformity