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66:
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172:
139:
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129:
119:
109:
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149:
39:
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but, which on further examination, were found to be a previously undescribed mineral.
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were sent to labs by S. A. Rust. Some specimens contained what appeared to be
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183:. It is a rare mineral first found in a limestone quarry near
231:
Clark, A. M.; Fejer, E. F.; Creesy, G; Tandy, P. C. (1988).
233:"Ashoverite, a new mineral, and other polymorphs of Zn(OH)
206:
The mineral was discovered after samples of the polymorph
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18:
191:, England, in 1988. It has also been found in the
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8:
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15:
7:
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237:from Milltown, Ashover, Derbyshire"
365:. You can help Knowledge (XXG) by
308:. You can help Knowledge (XXG) by
14:
432:Polymorphism (materials science)
349:
300:This article about a specific
264:10.1180/minmag.1988.052.368.14
1:
427:Minerals in space group 141
468:
437:Minerals described in 1988
344:
294:
452:Materials science stubs
281:Ashoverite Mineral Data
276:Handbook of Mineralogy
244:Mineralogical Magazine
67:Strunz classification
442:Oxide mineral stubs
422:Tetragonal minerals
357:This article about
256:1988MinM...52..699C
193:Harz mountain range
77:Dana classification
417:Hydroxide minerals
159:Optical properties
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359:materials science
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104:Colourless, milky
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283:, webmineral.com
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250:(368): 699–702.
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171:is one of three
150:Specific gravity
114:Perfect on {001}
45:
44:(repeating unit)
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447:Oxide minerals
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177:zinc hydroxide
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124:Vitreous, Dull
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96:Identification
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87:Crystal system
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412:Zinc minerals
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302:oxide mineral
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367:expanding it
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310:expanding it
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168:
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162:Uniaxial (+)
144:Translucent
140:Diaphaneity
406:Categories
287:Mindat.org
218:References
189:Derbyshire
173:polymorphs
169:Ashoverite
91:Tetragonal
57:IMA symbol
19:Ashoverite
199:, and in
208:sweetite
179:, Zn(OH)
110:Cleavage
81:6.2.11.1
29:Category
252:Bibcode
201:Namibia
197:Germany
185:Ashover
71:4.FA.10
40:Formula
33:Mineral
24:General
212:baryte
130:Streak
120:Luster
48:Zn(OH)
361:is a
304:is a
240:(PDF)
134:White
101:Color
363:stub
306:stub
260:doi
195:in
175:of
154:3.3
61:Aov
408::
258:.
248:52
246:.
242:.
203:.
187:,
394:e
387:t
380:v
369:.
337:e
330:t
323:v
312:.
266:.
262::
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235:2
181:2
50:2
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