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teaching - Earth Science Teachers' Association

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TEACHING EARTH SCIENCES ● Volume 26 ● Number 3, 2001<br />

a) b)<br />

Original Rocks<br />

Figure 1<br />

Example from the<br />

webpage:<br />

Fault Plane<br />

● Work out what the direction of movement is on this fault.<br />

Produce a labelled diagram of the fault, showing the direction of<br />

movement, and the evidence you used to work it out.<br />

If you are unsure about how to work out and mark the fault<br />

movement, click below for an explanation.<br />

EXPLANATION<br />

Normal Fault<br />

Extensional: rocks are<br />

pulled apart and upper<br />

block slides downwards<br />

Reverse Fault<br />

Compressional: rocks are<br />

squeezed together and upper<br />

block moves upwards. (Also<br />

called a thrust fault)<br />

Strike-slip Fault<br />

Rocks move horizontally. There<br />

may be a component of normal<br />

or-reverse movement:<br />

(oblique-slip) (Also called a<br />

wrench or tear fault)<br />

© Pamela Murphy 2001<br />

a) Left-hand frame:<br />

a photo-based<br />

exercise. If<br />

students need<br />

more information,<br />

they can click on<br />

the “explanation”<br />

button, which will<br />

bring up the<br />

information shown<br />

in (b).<br />

b) Right hand<br />

frame: a simple<br />

explanation of<br />

fault movement to<br />

help with the<br />

exercise.<br />

from South-West England, in order to link with a<br />

Kingston University first-year residential fieldtrip. However,<br />

knowledge of the regional geology is not necessary.<br />

Many of the photographs are active, and clicking on them<br />

allows users to zoom in for more detail of particular sections.<br />

In some examples, moving the mouse over a photo<br />

or graphic will bring up explanations of certain areas.<br />

Frequently Asked Questions<br />

The website is set out in fairly informal language, and<br />

uses the common web format of a FAQ (or Frequently<br />

Asked Questions) page to explain the background and to<br />

answer students’ common questions about notebooks.<br />

Examples include why they are being asked to draw<br />

things, or why some teachers or lecturers insist that they<br />

“ink in” their field notebook, while others insist they do<br />

nothing to it at all once they leave the field.<br />

Explanations<br />

Very little prior knowledge is assumed, and explanations<br />

are given of the geological features in the examples. For<br />

example, alongside an exercise requiring students to<br />

draw a diagram from a photograph of a fault, and to<br />

work out and mark the direction of movement, there is<br />

a link to a page explaining fault movement, and reverse<br />

versus normal faulting (see Figure 1). In another example,<br />

a labelled diagram of a fold shows features such as<br />

axial planar cleavage: students are asked to produce a<br />

similarly labelled diagram from a photo of another fold,<br />

identifying similar key features (see Figure 2).<br />

Simple animated graphics have been created to<br />

demonstrate dynamic processes, such as refolding of<br />

folds or the production of curved mineral fibres in<br />

veins through shearing.<br />

a) b)<br />

Fold Hinge<br />

Axial Plane<br />

Figure 2<br />

Example exercise<br />

from the website.<br />

Intersection<br />

of Cleavage<br />

on bedding<br />

Axial Planar<br />

Cleavage<br />

a) Explanation of<br />

the features within<br />

a fold.<br />

b) Exercise<br />

requiring students<br />

to produce a<br />

labelled diagram<br />

of a fold.<br />

Fold Axis<br />

Fold Limb<br />

© Pamela Murphy 2001<br />

● Using the diagram above, work out which features can be seen<br />

on the photo. Then make a labelled diagram of this fold.<br />

(Click on the photo to zoom in)<br />

103 www.esta-uk.org

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