<?xml version="1.0" encoding="utf-8" standalone="yes"?><rss version="2.0" xmlns:atom="http://www.w3.org/2005/Atom"><channel><title>Geometry on kenji.blog</title><link>http://kenji.blog/en/categories/geometry/</link><description>Recent content in Geometry on kenji.blog</description><generator>Hugo -- gohugo.io</generator><language>en</language><copyright>kenjinote</copyright><lastBuildDate>Thu, 10 Sep 2026 21:00:00 +0900</lastBuildDate><atom:link href="http://kenji.blog/en/categories/geometry/index.xml" rel="self" type="application/rss+xml"/><item><title>How Long Is the Coast of Britain?: The Coastline Paradox</title><link>http://kenji.blog/en/p/coastline-paradox/</link><pubDate>Thu, 10 Sep 2026 21:00:00 +0900</pubDate><guid>http://kenji.blog/en/p/coastline-paradox/</guid><description>&lt;img src="http://kenji.blog/p/coastline-paradox/img/coastline_paradox.jpg" alt="Featured image of post How Long Is the Coast of Britain?: The Coastline Paradox" />&lt;p>How many kilometers long is the coastline of Britain?
You might think the answer can be found in an encyclopedia or a geography textbook. However, in reality, there exists a strange fact: &lt;strong>&amp;ldquo;the answer changes depending on how you measure it, and theoretically becomes infinite.&amp;rdquo;&lt;/strong>&lt;/p>
&lt;p>This is the &lt;strong>Coastline Paradox&lt;/strong>. This discovery later sparked the creation of an entirely new field of mathematics called &amp;ldquo;fractal geometry.&amp;rdquo;&lt;/p>
&lt;h2 id="the-shorter-the-ruler-the-longer-the-distance">The Shorter the Ruler, the Longer the Distance
&lt;/h2>&lt;p>A coastline is not a straight line, but is composed of countless inlets, capes, and irregularities in the rocky surface.&lt;/p>
&lt;p>Suppose you measured the coastline of Britain with a giant 100 km ruler (a straight line). With this ruler, the jagged edges of small inlets and peninsulas under 100 km are ignored and shortcut.&lt;/p>
&lt;p>Next, let&amp;rsquo;s measure it again with a 1 km ruler. Since you are now measuring along the contours of the small bays and capes that were ignored earlier, the total length will inevitably be longer.&lt;/p>
&lt;p>Furthermore, what would happen if you measured the unevenness of every single rock with a 1 m ruler, the surface of pebbles with a 1 cm ruler, and the contours of grains of sand with a 1 mm ruler?&lt;/p>
&lt;div class="mermaid">graph TD
A["Measurement of Coastline"] --> B["100 km Ruler"]
A --> C["1 km Ruler"]
A --> D["1 m Ruler"]
B --> B1["Ignores small inlets"]
B1 --> B2["Measurement result: Approx. 2,800 km"]
C --> C1["Follows the shape of inlets"]
C1 --> C2["Measurement result: Approx. 3,400 km"]
D --> D1["Measures down to the unevenness of rocks"]
D1 --> D2["Measurement result: Increases further (theoretically infinite)"]
style B2 fill:#FFCDD2,stroke:#333
style C2 fill:#E57373,stroke:#333
style D2 fill:#F44336,stroke:#333,color:#fff&lt;/div>
&lt;p>Lewis Fry Richardson discovered this phenomenon empirically in 1951. As the unit of measurement (the length of the ruler) gets smaller, the measured length of the coastline increases endlessly.&lt;/p>
&lt;h2 id="fractal-dimension-between-1d-and-2d">Fractal Dimension: Between 1D and 2D
&lt;/h2>&lt;p>The mathematician Benoit Mandelbrot provided a mathematical explanation for this paradox. In 1967, he published a famous paper in the journal &lt;em>Science&lt;/em> titled &amp;ldquo;How Long Is the Coast of Britain? Statistical Self-Similarity and Fractional Dimension&amp;rdquo;.&lt;/p>
&lt;p>Mandelbrot pointed out that natural shapes like coastlines possess &lt;strong>self-similarity (fractals)&lt;/strong>, meaning that &amp;ldquo;no matter how much you zoom in, the same kind of complex structure appears.&amp;rdquo;&lt;/p>
&lt;p>If it were a pure mathematical straight line (1 dimension), the length would not change even if you halved the ruler. However, a coastline is so jagged that it is more complex than a 1D line, yet it is not a 2D surface with area either.&lt;/p>
&lt;p>Mandelbrot introduced the concept of &lt;strong>&amp;ldquo;fractal dimension (Hausdorff dimension)&amp;rdquo;&lt;/strong> to represent the complexity of such figures.
The fractal dimension of the coastline of Britain is estimated to be $D \approx 1.25$. In other words, the coastline of Britain is a mysterious entity with a &amp;ldquo;dimension higher than a 1D line, but lower than a 2D surface.&amp;rdquo;&lt;/p>
&lt;p>If the length of the ruler is $s$ and the measured length of the coastline is $L(s)$, the following relationship exists with the fractal dimension $D$:&lt;/p>
$$ L(s) \propto s^{1-D} $$
&lt;p>In the case of Britain&amp;rsquo;s coastline, $D = 1.25$, so $1 - D = -0.25$.
&lt;/p>
$$ L(s) \propto s^{-0.25} $$
&lt;p>
This shows mathematically that as the ruler length $s$ approaches 0, the measurement result $L(s)$ diverges to infinity $\infty$.&lt;/p>
&lt;h2 id="ultimate-conclusion-length-cannot-be-defined">Ultimate Conclusion: Length Cannot Be Defined
&lt;/h2>&lt;p>The concept of &amp;ldquo;length&amp;rdquo; that we use in everyday life works only for smooth straight lines and curves. Asking for the &amp;ldquo;absolute length&amp;rdquo; of a fractal figure existing in nature (coastlines, clouds, mountain ranges, branching of blood vessels, etc.) actually makes no mathematical sense.&lt;/p>
&lt;p>&amp;ldquo;How long is the coast of Britain?&amp;rdquo;
The correct answer is, &amp;ldquo;It depends on the length of the ruler used to measure it,&amp;rdquo; and theoretically, it is &amp;ldquo;infinite.&amp;rdquo; The fact that infinite length is folded into a limited small space can be said to be a beautiful paradox regarding our spatial perception.&lt;/p></description></item></channel></rss>