1.
g _ _ MAGNOHA
~- --—“"’L-; —- -I . . EDITIONS
Fina Ari Project:
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$yr0DliC discipline
synines-zing llflding
other sciences intoug
the conoepl oi Raum 3,
(area or spam)
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I The DEFINITION I ' ‘, .
II or GEOGRAPHY § V5,‘,
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jj has changed through Iimc, . Plolamy sf, . LOCATION Immnnual xi svumssis
Syr-mes-zmg aiscipime
to connect lhe general
wen im: SOCBJZII imough
measurement. mapping.
and a regmnal
emphasis
fqlril, |ll1(Y0ll"il'llin4ll Ilia. ‘
SCALE

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1. Discard much of the sky and foregro-un as reasonable. This is your initia crop.

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CEOHO
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2. The aim is to create four 1280x720 widescreen slides for a digital presentation. Set the vertical image size in Photoshop to 720 pixels, then
frame your four slides and discard the | eltover(s). Never alter the horizontal scale.
3. However, it is often beneficial to stretch the tiiertical scale or introduce some vertical exaggeration. So, go to Edit, Free Transfomi and stretch
the image vertically. This has the effect of making the viewpoint seem higher. It is the same technique that Al Lorenz (New York panoramas) and
H. C. Berann (Swiss Alps panoramas) used to such effect in the last century.
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6.
4. Some people will prefer a level horizon so now is the time to fix any
blemishes before the panorama is cut up into four.
Duplicate the panorama layer, and remove the right hand slides.
Select free transform and stretch the offending outer edge.
Flatten image and save changes.
If the innerjoins need attention, always start at the centre and work outwards
towards the edge.
5. Duplicate the panorama four times and create four separate 1280x720
slides.

7.
7. The slides can also be annotated, either individually or in groups.
By using a perspective style, the summary slide can also be used to
annotate individual themes.

8.
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10.
7. The slides can also be annotated, either individually or in groups.
By using a perspective style, the summary slide can also be used to
annotate individual themes.

11.
MENTEITHAGLACILI‘-DR
. ,
11,000 to 10,000 years ago, there was a
(last) readvance of valley glaciers down into the
Central Lowlands of Scotland. The evidence for this readvance
is provided by a complex but clear pattern of terminal moraine around
the southern shore of Loch Lomond and between the Port of Menteith and
Arnprior in the Forth Valley.

12.
THE LOCI‘!
The ice receded to reveal distinctive moraine belts.
REAEVAN G E
Lllanl tear iauii
The ~mii- is .
composed oi a series
oi pun. moraines V
flu ‘hn| e" In nu lake
basin which pmviaed
mo materlxlnlo form mo
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13.
TH= lE LAKE ©lF‘ iii EMTEUTFH a an example ©li‘ a l}iiilllallii<c: >>ll<e pair?
/ Lateral tear fault
Port of Menteith H, . Em‘ A A 7 Direction of ice
movement The “hill” is
composed of a series
cm can’ A7 , .
’. of push moraines
V: ::, < ‘ ‘°
-3&2!‘
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§ Lovwcnd Home __
if ,3 The_ “hole” is the_| ake
<3; ‘* basin which provided
the material to form the
it ' ll
hill
after Benn & Evans, Glaciers and Glacialion, 2010