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Natural Fractals PowerPoint Presentation
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Natural Fractals

Natural Fractals

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Natural Fractals

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  1. Natural Fractals (All underlines are links.) in and around Grand Canyon National Park

  2. When something is fractal… …little parts resemble big parts, called similarity… …substructure is present: similar shapes that repeat on different scales… …what shape the parts are depends entirely on the object.

  3. Fractals possess scale-invariance: scale-invariance implies a frame of reference is needed to determine size. • Fractals reveal symmetry under magnification: zooming in on a fractal object leaves the shape approximately unaltered. • Fractals have intersections with chaos theory: some processes are fractal and not chaotic, other processes are chaotic and not fractal, and some are both. • Fractals have non-integer dimension: see an example related to galaxies. • It can be difficult to make distinctions between • things that are fractals and: “things that look like fractals but aren’t.”

  4. Topics and other Pertinent Information: All underlines in the presentation are links. On slides 5-11, beneath the title of each topic is a link to its respective slides. I have tried to make it easy to jump between topics as an alternative to viewing the presentation in order. A word of caution: information is cumulative, with multiple references to previous slides. Slide notes pertaining to specific slides are located on my website and can be accessed by clicking on the Sierpinski triangle located in the bottom-right corner of every slide. If you want to use the notes and will not have web access, you can print them out ahead of time (about 30 pages). General directions for getting around in the slideshow and using the slides as slates to write on are located in the speaker notes inside the presentation. Right-click to access this general information at any time. You might try it now, right click, go either to Speaker Notes, or to Screen then Speaker Notes. They are the same on all slides.

  5. the Canyon Slides 12-55 Also visit:Fractal Terrain Modeling

  6. clouds Slides 56-61 the Canyon

  7. clouds trees Slides 62-90 the Canyon

  8. clouds lightning Slides 91-94 trees the Canyon

  9. clouds boundaries lightning Slides 95-109 trees the Canyon

  10. clouds rocks (frames of reference) lightning Slides 110-116 boundaries trees the Canyon

  11. clouds snowflakes lightning Slides 117-123 boundaries trees the Canyon rocks

  12. the Canyon

  13. striking examples of similarity can be seen even in hazy images of Grand Canyon, once you know what to look for Trail Overlook at dusk November 30, 2002

  14. look for shapes within shapes

  15. and here and here it’s here and here and here learn to recognize similarity:

  16. …in the Canyon specifically …in Nature generally

  17. This pattern will be the focus for the duration of the Canyon section. 18

  18. 19

  19. A pattern of mutually orthogonal joints runs throughout Grand Canyon, shown to me by Paul Knauth, Professor of Geology at Arizona State University.

  20. The joints form cracks--revealed through weathering--that separate the rock into blocks, that reveal more cracks through weathering, that cause separation into more blocks, in an ongoing process.

  21. Notice the blocky, rectilinear pattern. Think of corners in a room where three walls come together.

  22. There are other ways to see the joints… …you might prefer to look for lines…

  23. horizontal lines

  24. vertical lines

  25. blunt faces

  26. Lots of lines, blocks, and blunt faces to see here. .

  27. .

  28. Someday, this section will break off, probably right around this spot, following the blunt pattern seen throughout the Canyon.

  29. blunt face on Canyon wall …blunt face underfoot.

  30. Evidence of joints can be seen at the Rim, both underfoot and along the edge.

  31. many lines are at off-angles as well

  32. Desert View Drive

  33. 42

  34. …in big views of the Canyon, seek out repeating shapes…

  35. …for instance, rectangles

  36. …take a look at this loose block

  37. Now tilted, the surface of this block was originally horizontal.

  38. Look for evidence of falling (and fallen) blocks

  39. …a myriad of falling blocks resulting from joint erosion