Seashell surface

<h2 id="parametrization">Parametrization</h2>
<p>The following is a parameterization of one seashell surface:
</p>

=
                
                  
                    5
                    4
                  
                
                
                  (
                  
                    1
                    −
                    
                      
                        v
                        
                          2
                          π
                        
                      
                    
                  
                  )
                
                cos
                ⁡
                (
                2
                v
                )
                (
                1
                +
                cos
                ⁡
                u
                )
                +
                cos
                ⁡
                2
                v
              
            
            
              
            
            
              
                y

=
                
                  
                    5
                    4
                  
                
                
                  (
                  
                    1
                    −
                    
                      
                        v
                        
                          2
                          π
                        
                      
                    
                  
                  )
                
                sin
                ⁡
                (
                2
                v
                )
                (
                1
                +
                cos
                ⁡
                u
                )
                +
                sin
                ⁡
                2
                v
              
            
            
              
            
            
              
                z

=
                
                  
                    
                      10
                      v
                    
                    
                      2
                      π
                    
                  
                
                +
                
                  
                    5
                    4
                  
                
                
                  (
                  
                    1
                    −
                    
                      
                        v
                        
                          2
                          π
                        
                      
                    
                  
                  )
                
                sin
                ⁡
                (
                u
                )
                +
                15
              
            
          
        
      
    
    {\displaystyle {\begin{aligned}x&{}={\frac {5}{4}}\left(1-{\frac {v}{2\pi }}\right)\cos(2v)(1+\cos u)+\cos 2v\\\\y&{}={\frac {5}{4}}\left(1-{\frac {v}{2\pi }}\right)\sin(2v)(1+\cos u)+\sin 2v\\\\z&{}={\frac {10v}{2\pi }}+{\frac {5}{4}}\left(1-{\frac {v}{2\pi }}\right)\sin(u)+15\end{aligned}}}

<p>where 
  
    
      
        0
        ≤
        u
        <
        2
        π
      
    
    {\displaystyle 0\leq u<2\pi }
  
 and 
  
    
      
        −
        2
        π
        ≤
        v
        <
        2
        π
      
    
    {\displaystyle -2\pi \leq v<2\pi }
  
\\
</p><p>Various authors have suggested different models for the shape of shell. <a href="/facts/David_M._Raup/Iwj6G1KJ">David M. Raup</a> proposed a model where there is one magnification for the x-y plane, and another for the x-z plane. Chris Illert<a class="footnote-ref" id="fnref:1" href="#fn:1"><sup>1</sup></a> proposed a model where the magnification is scalar, and the same for any sense or direction with an equation like
</p>

F
              →
            
          
        
        
          (
          
            θ
            ,
            φ
          
          )
        
        =
        
          e
          
            α
            φ
          
        
        
          (
          
            
              
                
                  
                    cos
                    ⁡
                    
                      (
                      φ
                      )
                    
                    ,
                  
                
                
                  
                    −
                    sin
                    ⁡
                    (
                    φ
                    )
                    ,
                  
                
                
                  
                    
                      0
                    
                  
                
              
              
                
                  
                    sin
                    ⁡
                    (
                    φ
                    )
                    ,
                  
                
                
                  
                    cos
                    ⁡
                    
                      (
                      φ
                      )
                    
                    ,
                  
                
                
                  0
                
              
              
                
                  
                    0
                    ,
                  
                
                
                  
                    
                      0
                      ,
                    
                  
                
                
                  1
                
              
            
          
          )
        
        
          
            
              F
              →
            
          
        
        
          (
          
            θ
            ,
            0
          
          )
        
      
    
    {\displaystyle {\vec {F}}\left({\theta ,\varphi }\right)=e^{\alpha \varphi }\left({\begin{array}{*{20}c}{\cos \left(\varphi \right),}&{-\sin(\varphi ),}&{\rm {0}}\\{\sin(\varphi ),}&{\cos \left(\varphi \right),}&0\\{0,}&{\rm {0,}}&1\\\end{array}}\right){\vec {F}}\left({\theta ,0}\right)}

<p>which starts with an initial generating curve 
  
    
      
        
          
            
              F
              →
            
          
        
        
          (
          
            θ
            ,
            0
          
          )
        
      
    
    {\displaystyle {\vec {F}}\left({\theta ,0}\right)}
  
 and applies a rotation and exponential magnification.
</p>
<h2 id="see-also">See also</h2>
<ul><li><a href="/facts/Helix/BqC4AKwL">Helix</a></li>
<li><a href="/facts/Seashell/5AyVlBwo">Seashell</a></li>
<li><a href="/facts/Spiral/4R331aba">Spiral</a></li></ul>

<ul><li><a href="/facts/Eric_W._Weisstein/FbMuVDep">Weisstein, Eric W.</a> <a href="https://mathworld.wolfram.com/Seashell.html">"Seashell"</a>. <i><a href="/facts/MathWorld/yc1jodbq">MathWorld</a></i>.</li>
<li>C. Illert (Feb. 1983), "the mathematics of Gnomonic seashells", Mathematical Biosciences 63(1): 21-56.</li>
<li>C. Illert (1987), "Part 1, seashell geometry", Il Nuovo Cimento 9D(7): 702-813.</li>
<li>C. Illert (1989), "Part 2, tubular 3D seashell surfaces", Il Nuovo Cimento 11D(5): 761-780.</li>
<li>C. Illert (Oct 1990),"Nipponites mirabilis, a challenge to seashell theory?", Il Nuovo Cimento 12D(10): 1405-1421.</li>
<li>C. Illert (Dec 1990), "elastic conoidal spires", Il Nuovo Cimento 12D(12): 1611-1632.</li>
<li>C. Illert & C. Pickover (May 1992), "generating irregularly oscillating fossil seashells", IEE Computer Graphics & Applications 12(3):18-22.</li>
<li>C. Illert (July 1995), "Australian supercomputer graphics exhibition", IEEE Computer Graphics & Applications 15(4):89-91.</li>
<li>C. Illert (Editor 1995), "Proceedings of the First International Conchology Conference, 2-7 Jan 1995, Tweed Shire, Australia", publ. by Hadronic Press, Florida USA. 219 pages.</li>
<li>C. Illert & R. Santilli (1995), "Foundations of Theoretical Conchology", publ. by Hadronic Press, Florida USA. 183 pages plus coloured plates.</li>
<li>Deborah R. Fowler, Hans Meinhardt, and Przemyslaw Prusinkiewicz. Modeling seashells. Proceedings of SIGGRAPH '92 (Chicago, Illinois, July 26–31, 1992), In Computer Graphics, 26, 2, (July 1992), ACM SIGGRAPH, New York, pp. 379–387.<a href="http://algorithmicbotany.org/papers/shells.sig92.html">[1]</a></li>
<li>Callum Galbraith, Przemyslaw Prusinkiewicz, and Brian Wyvill. Modeling a Murex cabritii sea shell with a structured implicit surface modeler. The Visual Computer vol. 18, pp. 70–80. <a href="http://algorithmicbotany.org/papers/murex.tvc2002.html">http://algorithmicbotany.org/papers/murex.tvc2002.html</a></li></ul>

<h2 id="references">References</h2>

<ol>
<li id="fn:1"><p>Dr Chris Illert was awarded his Ph.D. on 26 September 2013 at the University of Western Sydney http://www.uws.edu.au/__data/assets/image/0004/547060/2013_ICS_Graduates.jpg. <a href="http://www.uws.edu.au/__data/assets/image/0004/547060/2013_ICS_Graduates.jpg" target="_blank">http://www.uws.edu.au/__data/assets/image/0004/547060/2013_ICS_Graduates.jpg</a> <a href="#fnref:1" class="footnote-back-ref">↩</a></p></li>
</ol>

Seashell surface open-in-new

Seashell surface