Hexagonal system - Revision history

Aschlafly: Reverted edits by NJrepublican (Talk) to last revision by BrianCo

2010-06-22T14:40:36Z

Reverted edits by NJrepublican (Talk) to last revision by BrianCo

NJrepublican: Redirected page to ASSFLY JUST LOOVVVVVVVEEEEEEEEESSSSSSSS Z'S MASSIVE COCK

2010-06-22T14:21:57Z

Redirected page to ASSFLY JUST LOOVVVVVVVEEEEEEEEESSSSSSSS Z'S MASSIVE COCK

BrianCo: removed trigonal

2007-07-15T17:01:14Z

removed trigonal

BrianCo: move & format

2007-07-15T16:10:30Z

move & format

New page

The '''hexagonal''' (or '''trigonal''') [[crystal system]] has four [[Axis|axes]] of [[symmetry]]: three, of equal length, lie in a plane at 120°; the fourth axis is longer or shorter and is at [[right angle]]s to the others.

[[Crystals]] are generally [[prismatic]] or [[columnar]], with a rounded [[triangle|triangular]] or [[hexagon]]al cross section; characteristic forms are three- or six-sided [[prism]]s, [[pyramid]]s, and [[rhombohedron]]s. The very similar ''[[trigonal system]]'' is often included within the hexagonal system.

==Sources==
*Chesterman, Charles W. ''The Audubon Society Field Guide to North American Rocks and Minerals'', Alfred A. Knopf: New York (1987), ''pp. 33-34''

[[Category:Crystallography]]

← Older revision		Revision as of 14:40, June 22, 2010
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−	~~#REDIRECT~~ [[~~ASSFLY JUST LOOVVVVVVVEEEEEEEEESSSSSSSS Z~~'~~S MASSIVE COCK~~]]	+	The '''hexagonal''' [[crystal system]] has four [[Axis\|axes]] of [[symmetry]]: three, of equal length, lie in a plane at 120°; the fourth axis is longer or shorter and is at [[right angle]]s to the others.
		+
		+	[[Crystals]] are generally [[prismatic]] or [[columnar]], with an [[hexagon]]al cross section; characteristic forms are six-sided [[prism]]s. The similar [[trigonal system]] (or rhombohedral) is often included within the hexagonal system.
		+
		+	==Sources==
		+	*Chesterman, Charles W. ''The Audubon Society Field Guide to North American Rocks and Minerals'', Alfred A. Knopf: New York (1987), ''pp. 33-34''
		+
		+
		+	[[Category:Crystallography]]

← Older revision		Revision as of 14:21, June 22, 2010
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−	~~The '''hexagonal''' [[crystal system]] has four~~ [[~~Axis\|axes]] of [[symmetry]]: three, of equal length, lie in a plane at 120°; the fourth axis is longer or shorter and is at [[right angle]]s to the others.~~	+	#REDIRECT [[ASSFLY JUST LOOVVVVVVVEEEEEEEEESSSSSSSS Z'S MASSIVE COCK]]
−
−	[[Crystals]] are generally [[prismatic]] or [[columnar]], with an [[hexagon]]al cross section; characteristic forms are six-sided [[prism]]s. The similar [[trigonal system]] (or rhombohedral) is often included within the hexagonal system.
−
−	~~==Sources==~~
−	*Chesterman, Charles W. ''The Audubon Society Field Guide to North American Rocks and Minerals'', Alfred A. Knopf: New York (1987), ''pp. 33-34''
−
−
−	~~[[Category:Crystallography~~]]

@@ Line 1: / Line 1: @@
-The '''hexagonal''' (or '''trigonal''') [[crystal system]] has four [[Axis|axes]] of [[symmetry]]: three, of equal length, lie in a plane at 120°; the fourth axis is longer or shorter and is at [[right angle]]s to the others.
+The '''hexagonal''' [[crystal system]] has four [[Axis|axes]] of [[symmetry]]: three, of equal length, lie in a plane at 120°; the fourth axis is longer or shorter and is at [[right angle]]s to the others.
-[[Crystals]] are generally [[prismatic]] or [[columnar]], with a rounded [[triangle|triangular]] or [[hexagon]]al cross section; characteristic forms are three- or six-sided [[prism]]s, [[pyramid]]s, and [[rhombohedron]]s. The very similar ''[[trigonal system]]'' is often included within the hexagonal system.
+[[Crystals]] are generally [[prismatic]] or [[columnar]], with an [[hexagon]]al cross section; characteristic forms are six-sided [[prism]]s. The similar [[trigonal system]] (or rhombohedral) is often included within the hexagonal system.
 ==Sources==