Halos Of Stone

Inside the permafrost regions of the Arctic, soil and rocks are fashioned into strikingly beautiful and orderly patterns that have confronted geologists for centuries. Each summer, the retreating snows unveil a bizarre assortment of rocks arranged in a honeycomb like network as the ground begins to
thaw, giving the landscape the appearance of a tiled floor. These patterns are found in most of the northern lands and alpine regions, where the soil is exposed to moisture and seasonal freezing and thawing. The polygons range in size from some inches across when composed of small pebbles to numerous tens of feet when significant boulders form protective rings around mounds of soil.
The polygons had been possibly produced by forces similar to those that cause frost heaving, which pushes rocks up by way of the soil. This phenomenon is effectively known to northern farmers, as every single spring produces a new crop of stones in their fields. The boulders move by way of the soil either by a pull from above or by a push from below. If the leading of the rock freezes very first, it really is pulled up by the expanding frozen soil. When the soil thaws, sediment gathers below the rock, which settles at a slightly higher level. The expanding frozen soil lying below could also heave the rock upward. Following several freeze thaw cycles, the boulder finally rests on the surface. Rocks also have been identified to push through highway pavement, and fence posts happen to be shoved completely out of the ground by frost heaving.
The regular polygon patterned ground might happen to be formed by the movement of soil of mixed composition upward toward the center of the mound and downward below the boulders. The material moves down below the gravel in an action similar to that in a subduction zone. The soil might move in convective cells, significantly as bubbles rise up in a pot of boiling water. The coarser material, composed of gravel and boulders, is gradually shoved radially outward from the central region and subducted along the edges, leaving the finer materials behind. This idea is supported by the reality that the material inside the center of the mound typically appears churned up. The opposite condition occurs during the formation of stone pits, which are in each and every respect the inverse of stone polygons. Instead of convection cells circulating up through the center of the polygon and down along the borders, in stone pits the circulation is down by way of the center and up along the outside. The arctic soil provides an assortment of other geometric designs, including methods, stripes, and nets that lie among the circles and polygons. These forms can reach 150 feet in diameter. Relics of ancient surface patterns shaped during the last ice age measuring up to 500 feet have been found in former permafrost regions. Even images of Mars sent back from spacecraft depict furrowed rings, polygonal fractures, and ground-ice patterns of every description, suggesting that the planets surface water has long because gone underground.
Other examples of patterned ground include polygonal shapes created in desert muds, which had been formed by the contraction of the mud when it dried rapidly inside the hot Sun. Sorted circles also might form by the increased wearing down of coarse grains in isolated cracks in bedrock. Even vibrations from earthquakes are thought to cause the sorting of some sediments. Pebbles embedded in sand rise toward the surface during ground shaking as a result of convective motions inside the sediment. Vibrating sands in the surface congregate into stable patterns, including hexagons, squares, stripes, and circular heaps. Also, curious occurrences of patterns form in sediments on the ocean floor.

Joseph Kieffer
http://jewelryuk.org
from: http://hand-crafted-jewelry.com

Trackback URL

No Comments on "Halos Of Stone"

Hi Stranger, leave a comment:

ALLOWED XHTML TAGS:

<a href="" title=""> <abbr title=""> <acronym title=""> <b> <blockquote cite=""> <cite> <code> <del datetime=""> <em> <i> <q cite=""> <strike> <strong>

Subscribe to Comments