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Key facts
Witherite (BaCO3) ã¯ãç¬ç¹ãªç䌌å è§æ¶ã®åæ¶ãšéç«ã€èå ã§ã³ã¬ã¯ã¿ãŒã«æãç¥ãããçé žããªãŠã ã®çš®ã§ããçŽæ¹æ¶ç³»ã§ãããªãããäžã€çµïŒããã³åŸªç°çåæ°ïŒãšããŠééåæ¶ããã°ãã°åœ¢æããå è§æ±ãšãå èæããæš¡ããŸããçµæ¶ã¯éåžžçœè²ããã¯ãªãŒã è²ã§ãæã«ã¯ç°è²ããã£ããæ·¡ãèèè²ã«ãªãããšããããã¬ã©ã¹å æ²¢ããããã·ã«ããŒãªå æ²¢ãæããŸãïŒéŸä¹³ç¶ããã³æ¿ç¶ã®æé·ãå®çªã§ãã ãã®çš®ã¯çé žå¡©ã®äžã§ãç¹ã«å¯åºŠãé«ããäœæž©ã®ç±æ°Žèã§èç³ãæ¹éé±ãéäºéé±ãæ¹è§£ç³ããã©ã€ããšãšãã«çŸããããšãå€ãã§ãã
æãæåãªãŠã£ã¶ã©ã€ãæšæ¬ã¯ãåã€ã³ã°ã©ã³ãã®ããã³å±±èã®é±èå°åž¯ãç¹ã« Settlingstones é±å±±ãš Alston Moor é±å±±ããã§ãå¯Ÿç §çãªåºè³ªã®äžã«ããã·ã£ãŒãã§åœ«å»çãªåæ¶çµæ¶ã代ã ãã®çš®ãå®çŸ©ããŠããŸãããå€ãã®è±ç£äŸã¯çæ³¢UVäžã§çœè²ããéçœãèå ãïŒäžã«ã¯çå ãæŸã€ãã®ããããŸãïŒããŠã£ã¶ã©ã€ãã¯åžžå äžã§ãUVç¯äžã§ãèŠ³è³æ§ã®é«ãæšæ¬ã§ããäžè³ªãªæšæ¬ã¯çšã§ãæè¿ã®å ¥æã¯ãŸããŸãå°é£ã§ããå æ²¢ã®è¯ãåæ¶ã§ãUVåå¿ã匷ããé åçãªåºè³ªãåãããã®ã¯é«å€ã§ååŒãããŸãã
Witherite ã¯é奜ã¿ã®çé žå¡©ã§ããæŽŸæãªçš®ã瀺ãè¹è²ã«ã¯åã°ãªããã®ã®ããã®ç¬ç¹ãªåæ¶åœ¢ç¶ãè±åœã«ãããæŽå²çãªç³»èããããŠçãçããšããèå ããå®å®ããéèŠãä¿ã£ãŠããŸããæ¬§å·ã®åç©é€šãã¯ã©ã·ãã¯ã³ã¬ã¯ã·ã§ã³ã«ã¯ãæç§æžç㪠Settlingstones ã®åæ¶ãå«ãŸããããšãå€ããäžçŽã³ã¬ã¯ã¿ãŒã¯ Nentsberry HaggsãTynebottomãBrownley HillãDry Gill ãªã©ã® Alston Moorç£ã®çŸããåºè³ªä»ãæšæ¬ãæ¢ããŸãã
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Arguably the worldâs most famous witherite locality, Settlingstones (Northumberland) produced iconic pseudo-hexagonal twins and cyclic multiples with excellent luster and translucency. Many show crisp faces and sharp terminations in stacked groupings, often perched on fluorite-bearing matrix. Under shortwave UV these crystals typically glow a brilliant bluish-white, sometimes with a lingering phosphorescence. The combination of form, size, and fluorescence set the standard; intact matrix specimens with few or no dings are the benchmark for the species.
Nentsberry Haggs is renowned for stout, well-formed witherite twins with a slightly satiny luster, frequently set among sulfides and fluorite for strong contrast. Compared with Settlingstones, crystals here can look a touch more massive but remain highly aesthetic. Many pieces fluoresce powerfully under SW UV. Older classic specimens from 19thâ20th century finds are now scarce; undamaged terminations and balanced arrangements elevate value significantly.
An important historical source, Fallowfield produced handsome witherite twins and aggregates, sometimes with a warm cream tone and a satiny sheen. Fluorite and galena associations are common. While production was never as prolific as Settlingstones, choice pieces represent quintessential English witherite and are well regarded for their old-mine character and strong UV activity.
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