Needle ice

Needle Ice forming in a pile of red clay soil
Needle ice pushing up soil particles
Needle ice is formed of distinct, unconsolidated strands

Needle ice is a needle-shaped column of ice formed by groundwater. Needle ice forms when the temperature of the soil is above 0 °C (32 °F) and the surface temperature of the air is below 0 °C (32 °F). Liquid water underground rises to the surface by capillary action, and then freezes and contributes to a growing needle-like ice column. The process usually occurs at night when the air temperature reaches its minimum.

The ice needles are typically a few centimetres long. While growing, they may lift or push away small soil particles. On sloped surfaces, needle ice may be a factor contributing to soil creep.[1][2]

Alternate names for needle ice are "frost pillars" ("Säuleneis" in German), "frost column", "Spew Ice", "Kammeis" (a German term meaning "comb ice"), "Stängeleis" (another German term referring to the stem-like structures), "shimobashira" (霜柱, a Japanese term meaning frost pillars), or "pipkrake" (from Swedish pipa (tube) and krake (weak, fine), coined in 1907 by Henrik Hesselman).[3]

The similar phenomena of frost flowers and hair ice can occur on living or dead plants, especially on wood.

  1. ^ Isbell, D.: Needle Ice on Mt. Osceola Archived 2006-05-27 at the Wayback Machine, EPOD of July 10, 2005. URL last accessed 2007-12-07.
  2. ^ Pidwirny, M.: Fundamentals of Physical Geography, 2nd ed., section 10(ag), Periglacial Processes and Landforms. URL last accessed 2007-12-07.
  3. ^ Lawler, D. M.: "Some observations on needle ice", Weather, vol. 44, pp. 406–409; 1989.