# Ancient Web: Kenneth Libbrecht Explained Why Snowflakes Branch

Kenneth Libbrecht's Caltech-hosted SnowCrystals.com essay uses plain hypertext and small diagrams to explain ice dendrites, snowflake branching, and crystal growth.

2026-10-04
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Switchboard Tech Services


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Part of the [Ancient Web Collection](https://switchboardtechservices.com/articles/ancient-web-collection/).

The six-armed snowflake looks like somebody designed it with a drafting compass. It is actually the result of water molecules finding tiny advantages as ice grows.

[Visit the Snowflake Branching page](https://www.its.caltech.edu/~atomic/snowcrystals/dendrites/dendrite.htm)

This compact science lesson is part of **[SnowCrystals.com](http://SnowCrystals.com)**, a project by **Kenneth G. Libbrecht** at Caltech. The page footer contains an old visitor counter labeled as counting views since **February 1, 1999**, tying the collection's public-Web presentation to the late 1990s.

The site has a decidedly early-Web layout: a long sidebar of small, descriptive links to natural snowflakes, laboratory-grown crystals, historic photographs, ice halos, snowflake physics, and activities for children. What survives is not merely a static photograph album but a set of independent explanations that can be followed in any order.

## A tiny bump turns into a branch

The [branching article](https://www.its.caltech.edu/~atomic/snowcrystals/dendrites/dendrite.htm) explains the surprising physics in ordinary words. Water vapor has to diffuse through the air before freezing onto an ice crystal. A bump extending slightly beyond a flat ice surface can reach those molecules more easily. Because it grows faster, the bump gets still farther ahead, giving its next growth another advantage.

Libbrecht calls this feedback a **branching instability**. Repetition creates smaller branches off larger branches, producing the tree-like forms called **dendrites**. The lesson describes how reduced air pressure means easier diffusion and fewer branches, while higher pressure can increase branching.

There is a second force too: **faceting**, which favors simple, flat crystal faces. A snowflake's final shape depends on the balance between faceting and branching, changing with temperature and humidity.

The site's navigation leads to [an introductory snowflake primer](https://www.its.caltech.edu/~atomic/snowcrystals/primer/primer.htm), [a guide to natural crystal types](https://www.its.caltech.edu/~atomic/snowcrystals/class/class.htm), and laboratory-grown 'designer' snowflakes. Those accompanying pages put the short branching essay inside a much larger public-science effort, even if not every image or legacy link is guaranteed to work in a modern browser.

Its historical value is the form as much as the content: a scientist could put a genuinely useful lesson on a university-hosted page and connect it to dozens of examples without making visitors join a course.

[Read the original snowflake branching explanation](https://www.its.caltech.edu/~atomic/snowcrystals/dendrites/dendrite.htm).

Part of the [Ancient Web Collection](https://switchboardtechservices.com/articles/ancient-web-collection/).

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Author: Switchboard Tech Services

Published: 2026-10-04T13:51:21+00:00

Modified: 2026-10-18T21:03:40.040135+00:00
