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Planet Panorama

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Photoshop for geographers. An examination of the Highland Boundary Zone in Scotland using design techniques to improve the learning experience.

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Planet Panorama

  1. 1. g _ _ MAGNOHA ~- --—“"’L-; —- -I . . EDITIONS Fina Ari Project: . Z — I . ... ..au4.. ... _ m .14 1-"
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  3. 3. $yr0DliC discipline synines-zing llflding other sciences intoug the conoepl oi Raum 3, (area or spam) The puiposn oi gear; -.iprI, “, ’ l0[iIi. K1r* it Im Tl rm MVITIVJ I-; .mI a, m. .mrI3 Ilia ioc. I:Ion of was I = :” -. ‘.. , , f, I The DEFINITION I ' ‘, . II or GEOGRAPHY § V5,‘, . ?g 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
  4. 4. c. :‘Ia[‘i'? ‘-~ r -. u.. IaLv' ; |. ’.»'-‘. -.7- o; .n"4-In. 4 . >~ 1. Discard much of the sky and foregro-un as reasonable. This is your initia crop.
  5. 5. CEOHO W. .. .7 L. «.-_. ..». .. s<, Y>. ,‘V>g4V4.- —: ,__. ... __ . _ -2- ‘V ‘ -5 ~_ ' ‘ - _' 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. 4 . L.. -»J . '
  6. 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. 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.
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  9. 9. _ -—~-—. ... . --4 *8*"""“'1". "~V! a'r--~, ... - . ... .
  10. 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. 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. 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 . .,. I.
  13. 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!‘ 'r6 .21 A rrrr (N ‘ x 8 Box "V, 9 . § 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

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