Tag Archives: amaminerali

Kungani Wonke Lawo Matshe Nezimbiwa Egcina “nge-ite”?

Kungani Wonke Lawo Matshe Nezimbiwa Ephela "ku-ite"

Wake wazibuza ukuthi kungani amagama amaningi amaminerali egcina ngohlamvu “ite”? Le ndlela yolimi ayiyona into eyenzeka ngengozi, futhi ihambisana nomlando ocebile osukela ezikhathini zasendulo. Ukungena ku-etymology yamagama amaminerali kufana nokuhlola i-geological ngokwayo, okwembula izingqimba zamasiko kanye nentuthuko yesayensi eyakha ulimi lwamagugu oMhlaba.

Ukubuka Kwedlule

Isijobelelo “ite,” elizwakalayo nelijwayelekile, liye lanamathiselwa emagameni amaminerali amaGreki futhi kamuva amaRoma. Lezi zimpucuko zisebenzisa iziphetho “izinto” kanye nethi “itis” ukukhombisa izimfanelo, ukusetshenziswa, izakhi, or izindawo ezihlobene namaminerali namatshe. Ngokwesibonelo, igama elithi “siderites,” manje elaziwa ngokuthi siderite, elisuselwa egameni lesiGreki elisho insimbi, laqanjwa ngenxa yensimbi yalo. Ngokufanayo, i-“hematites” (manje eyi-hematite) yathatha inkomba yayo egameni legazi ngenxa yombala obomvu oboniswa lapho i-mineral iyimpushana.

Ukusuka ku-Lite kuya ku-Ite

Ezikhathini zasendulo, lezi zimiso zokuqamba zazisetshenziswa ngokungaguquki, ngaphandle kwamagama abantu. Kukholakala ukuthi isiphetho esithi “lite” sisuka kusijobelelo sesiFulentshi esithi “lithe,” okusho ukuthi, sisuka ku “lithos,” igama lesiGreki elisho itshe. Kwesinye isikhathi, isiphetho esithi "lite" sasingahle kube ukusebenziseka kolimi, okwenza amagama aphimisele kalula.

Ngale Kwejwayelekile

Nakuba i-“ite” isalokhu ihamba phambili, ezinye iziphetho nazo zengeze ukuthinta okumnandi kusichazamazwi samaminerali. Isiphetho "ine" siyanikeza us amaminerali afana ne-olivine, i-tourmaline, ne-nepheline. I-“Ane” ikhona ku-cymophane, kuyilapho i-“ase” ikhanya phakathi i-dioptase, i-euclase, ne-orthoclase. Bese kuba khona “yre,” etholakala ku-dipyre engavamile.

Ukuzibandakanya neGugu lethu leGeological

Ukuqonda imvelaphi yamagama amaminerali akuyona nje umsebenzi wezemfundo; kusixhumanisa nefa lobuhlakani bempucuko edlule. Amagama angamathuluzi e-mnemonic ahlanganisa ingqikithi yamaminerali, umlando wayo, futhi, ngezinye izikhathi, ukusetshenziswa kwayo. Kubantu abanelukuluku lokwazi kanye nabafundi abashisekayo, lawa magama ayisango eliya ezweni elimangalisayo nelinemibala engaphansi kwezinyawo zethu.

Ngezansi kunethebula elibonisa amaminerali namatshe ahehayo angu-50 agcina “ngento” ewumlingo, esimema ukuthi sihlole izinganekwane zawo ezifihliwe kanye nokubaluleka kokwakheka komhlaba.

Amaminerali Adumile Aphela 'nge-ite'Ama-Rocks adumile agcina nge-'ite'
I-QuartziteI-Amphibolite
IHaliteI-basaltite
FluoriteI-Dacite
I-CalciteRhyolite
UzibutheIphonolite
IHematiteI-Obsidianite
I-AragoniteI-trachyte
I-BariteI-Pumicite
I-PyriteI-Chertite
SphaleriteComendi
I-BiotiteI-Pantellerite
MuscoviteI-Theralite
I-AlbiteNamuhla
I-CelestiteAndesite
I-garnetite (igama ngezinye izikhathi elisetshenziselwa amadwala acebile nge-garnet)I-Trondhjemite
I-DolomiteI-Anorthosite
I-ChalcopyriteDunite
malachiteI-Foidolite
kyaniteIjolite

I-Peridot: Umhlahlandlela Ophelele Wezazi Zomhlaba

ikristalu ye-peridot

I-Peridot iyitshe eliyigugu elihle osekunesikhathi laziswa ngombala walo oluhlaza ogqamile. Kodwa kuma-geologists, i-peridot ibamba ukuthakazelisa okukhethekile ngenxa yezakhiwo zayo eziyingqayizivele nokubaluleka kokwakheka komhlaba. Kulo mhlahlandlela ophelele, sizohlola izakhiwo ze-peridot, yayo ukuqeqeshwa kanye nokuvela emvelweni, kanye nokubaluleka kwayo emkhakheni wegeology.

I-Peridot iwuhlobo lwamaminerali aziwa ngokuthi i-olivine, eyenziwe ngezinto ezihlukahlukene ezihlanganisa insimbi, i-magnesium, ne-silicon. Ivame ukutholakala emadwaleni avuthayo njenge-basalt ne-gabbro, futhi ngokuvamile ihlotshaniswa nenqubo ye-plate tectonics. Eqinisweni, i-peridot ivame ukwakhiwa ngenxa yokushisa okukhulu nokucindezela ngaphakathi koqweqwe lomhlaba, okuyenza ibe ithuluzi elibalulekile lezazi zokwakheka komhlaba ezifunda umlando womhlaba nezinqubo zangaphakathi.

Esinye sezici ezihluke kakhulu ze-peridot umbala wayo oluhlaza ogqamile, obangelwa ukuba khona kwensimbi. Lo mbala ungahluka ukusuka kokuphuzi okuluhlaza kuya koluhlaza okotshani ojulile, futhi ngokuvamile uchazwa ngokuthi “okufana nepheya.” Ngaphezu kombala wayo, i-peridot nayo yaziwa ngayo ubulukhuni nokuqina, okwenza kube ukukhetha okudumile kobucwebe.

I-Peridot itholakala ezindaweni eziningi emhlabeni jikelele, ngezinye zediphozithi ezibalulekile ezitholakala ku- I-united states, China, kanye Pakistan. Itholakala futhi ngamanani amancane kwamanye amazwe anjengeBrazil, Norway, neRussia. E-United States, i-peridot ingatholakala ku Arizona, eyaziwa ngamatshe ayigugu acebile.

Njengetshe eliyigugu, i-peridot iye yaziswa amakhulu eminyaka futhi inomlando omude wokusetshenziswa ubucwebe nezinye izinto zokuhlobisa. Kuphinde kube yisinqumo esidumile sabaqoqi nabashisekayo ngenxa yezakhiwo zayo ezihlukile kanye nohlu olubanzi lwemibala. Kodwa-ke, kuma-geologists, i-peridot ingaphezu nje kwetshe eliyigugu elihle. Kuyithuluzi elibalulekile lokuqonda umlando woMhlaba nezinqubo zangaphakathi, futhi liyingxenye ebalulekile yomkhakha we-geology.

Sengiphetha, i-peridot iyiminerali ethokozisayo nebalulekile ebambe ukuthakasela okukhethekile kwezazi ze-geologists. Izici zawo eziyingqayizivele, ukuvela kwemvelo, kanye neqhaza emkhakheni we-geology kuwenza ube yingxenye ebalulekile yocwaningo loMhlaba nezinqubo zawo. Ukuthi uyisazi sokuma komhlaba or nje umthandi wamatshe ayigugu amahle, i-peridot iyimaminerali eqinisekile ukuthi izobamba ukunaka kwakho.

I-Geology Yethusi: Insimbi Ethakazelisayo Enomlando Ocebile

Ama-cubes ethusi ahlanzekile

Copper iyingxenye yamakhemikhali enophawu u-Cu kanye nenombolo ye-athomu engu-29. Iyinsimbi ethambile, ethambile, nedubulekayo ene-thermal ephezulu kakhulu kanye ne-electrical conductivity. I-Copper itholakala oqweqweni lomhlaba ezinhlobonhlobo zamaminerali, kufaka phakathi i-chalcopyrite, malachite, futhi bornite. Kuwo wonke umlando, iye yadlala indima ebalulekile empucukweni yabantu, kusukela ekuthuthukisweni kwamathuluzi nobucwebe kuya ekusetshenzisweni kwayo ezintanjeni zikagesi zesimanje. Kulokhu okuthunyelwe kwebhulogi, sizocubungula i-geology yethusi, sihlole yayo ukuqeqeshwa, izakhiwo, kanye nokusetshenziswa emhlabeni namuhla.

Ukwakhiwa Kwethusi

Ithusi liyinto evamile oqweqweni lomhlaba, okwenza isilinganiso esilinganiselwa ku-0.0001% wobunzima bomhlaba. Itholakala ezinhlobonhlobo zamaminerali, kanti i-chalcopyrite iyinala kakhulu futhi ibalulekile kwezomnotho. I-Copper ingatholakala futhi ngamanani amancane ngesimo somdabu, okusho ukuthi ayihlanganisiwe nezinye izakhi kumaminerali.

Amaminerali e-Copper akha ezindaweni ezihlukahlukene ze-geological, kuhlanganise ne-volcanic, sedimentary, kanye nemvelo ye-metamorphic. Amadiphozithi ethusi abaluleke kakhulu, noma kunjalo, yilezo ezakha kusuka ekuhlanganiseni kwethusi oketshezini olushisayo. Lolu ketshezi, olunothe ngamaminerali ancibilikisiwe, lukhiqizwa ngesikhathi sokupholisa nokuqiniswa kwetshe elincibilikisiwe, elaziwa ngokuthi i-magma.

Njengoba uketshezi luhamba oqweqweni lomhlaba, lungavaleleka ezingxenyeni eziqhekekile namaphutha, akhe imithambo yamaminerali ethusi. Amaminerali angaphinda afakwe edwaleni elinezimbotshana, njenge-sandstone, enze uhlobo lwediphozi eyaziwa ngokuthi i-porphyry copper deposit.

Izakhiwo Zethusi

I-Copper inenani lezinto eziyingqayizivele ezenza kube insimbi ebalulekile emisebenzini ehlukahlukene. Kuyi-conductor enhle yokushisa nogesi, okwenza kube usizo ekudluliseni ugesi kanye nokwakhiwa kwama-heaters. I-Copper ibuye imelane nokugqwala, iyenze ibe yinto ehlala isikhathi eside ukuze isetshenziswe kumapayipi nezinye izingqalasizinda.

Copper can be combined with other metals to form alloys, which can have improved strength, ubulukhuni, and other properties. Some common copper alloys include brass, which is a mixture of copper and zinc, and bronze, which is a mixture of copper and tin.

Ukusetshenziswa kwe-Copper

Ithusi selisetshenziswe abantu izinkulungwane zeminyaka, nobufakazi bokusetshenziswa kwalo kusukela empucukweni yasendulo yaseGibhithe, eChina naseMelika. Esikhathini esidlule, ithusi lalisetshenziselwa ukwenza amathuluzi, ubucwebe nezinto zokuhlobisa. Yayisetshenziswa futhi ekwakhiweni kwezakhiwo, njengoba iwumqhubi omuhle wokushisa nogesi.

Namuhla, ithusi lisetshenziswa ezintweni ezihlukahlukene, okuhlanganisa izintambo zikagesi, amapayipi amanzi, nokwakhiwa kwezimoto nezindiza. Ibuye isetshenziswe ekukhiqizeni izinhlamvu zemali, ubucwebe, nezinye izinto zokuhlobisa. I-Copper iyisici esibalulekile sama-alloys amaningi, kuhlanganise nethusi nethusi, asetshenziswa ezinhlobonhlobo zezicelo.

Ukumbiwa kwethusi nakho kuye kwafeza indima ebalulekile ekuthuthukisweni komphakathi wesintu. Izimayini zethusi zingatholakala ezindaweni ezihlukahlukene emhlabeni jikelele, kuhlanganise neChile, i I-united states, kanye ne-Australia. Ukumba ithusi kuhilela ukukhishwa kwensimbi emhlabeni, bese igaywa ukuze kukhiqizwe insimbi yethusi. Ukumbiwa kwekhopha kungaba nomthelela omkhulu kwezemvelo, okuhlanganisa ukukhishwa kwamakhemikhali anobuthi nokucekelwa phansi kwezindawo zokuhlala. Ngenxa yalokho, imboni yezimayini yenze imizamo yokunciphisa umthelela wayo kwezemvelo, okuhlanganisa nokuthuthukiswa kwezinqubo zokumba esimeme kanye nokusetshenziswa kwethusi eligaywe kabusha.

Isiphetho

I-Copper iyinsimbi ethakazelisayo enomlando ocebile kanye nokusetshenziswa okuhlukahlukene. Izakhiwo zayo eziyingqayizivele, kuhlanganise nekhono layo lokuqhuba ukushisa nogesi kanye nokumelana kwayo nokugqwala, kuyenza ibaluleke

insiza emphakathini wanamuhla. Kusukela ezintambo zikagesi namapayipi amanzi kuya ekwakhiweni kwezimoto nezindiza, ithusi lidlala indima ebalulekile ezicini eziningi zokuphila kwethu.

Naphezu kokubaluleka kwayo, ukumba ithusi kungaba nomthelela omkhulu kwezemvelo. Kubalulekile ukuthi imboni iqhubeke nokusebenzela izindlela zokumba ezinzile kanye nokusetshenziswa kwethusi eligaywe kabusha ukuze kuncishiswe le mithelela.

Kafushane, i-geology yethusi iyisihloko esithakazelisayo, lapho insimbi itholakala kumaminerali ahlukahlukene futhi yakheka ezindaweni ezihlukahlukene ze-geological. Izakhiwo kanye nokusetshenziswa kwayo kuyenza ibe yinsiza ebalulekile ezweni lanamuhla, futhi ukumba ithusi kube nendima ebalulekile emlandweni wesintu.

Ukuhlola Ubuhle Nomlando We-Carnelian: Umbono We-Geologist

i-carnelian palmstone

I-Carnelian iyiminerali ekhangayo ebilokhu ithakaselwa ngombala wayo omuhle obomvu osawolintshi amakhulu eminyaka. Kodwa bewazi yini ukuthi empeleni kuwuhlobo lwe-chalcedony, izinhlobonhlobo ze asebenza ngebhethri? Kulokhu okuthunyelwe kwebhulogi, sizohlola i-geology ye-carnelian futhi sifunde ngayo ukuqeqeshwa, izakhiwo, kanye nokusetshenziswa. Kusukela empucukweni yasendulo kuya ekuklanyweni kobucwebe besimanje, i-carnelian ibambe iqhaza elikhulu emlandweni wesintu. Ukuthi uyisazi sokuma komhlaba or umane ube a ukuthanda ngamatshe namaminerali, lokhu okuthunyelwe kuzohlinzeka ngokubheka okujulile emhlabeni othakazelisayo we-carnelian.

I-Carnelian iwuhlobo lwe-microcrystalline quartz, okusho ukuthi yenziwe ngamakristalu amancane, ahlanganiswe ngokuqinile. Yakheka ngenqubo yemvula ye-silica, eyenzeka lapho uketshezi olucebile nge-silica, njengamanzi angaphansi komhlaba, luhlangana nento engase isebenze njenge-nucleus yokukhula kwekristalu, njenge-fossil noma umgodi edwaleni. Ngokuhamba kwesikhathi, i-silica emanzini izokhula kancane futhi yakhe ikristalu.

I-Carnelian ivame ukutholakala ngokuhlanganyela nezinye izinhlobo ze-quartz, njenge agathe kanye nekhalkedoni. Ibonakala ngombala wayo oyingqayizivele osawolintshi-obomvu, obangelwa ukuba khona kwe-iron oxide kumaminerali. Ubukhulu bombala bungahluka ukusuka kokuwolintshi ophaphathekile kuye kobomvu ojulile, obunjengomlilo, kuye ngenani le-iron oxide ekhona. I-Carnelian yaziwa nangokuguquguquka kwayo kanye nendlela ebonakala ikhanya ngayo ngaphakathi.

I-Carnelian inomlando omude wokusetshenziswa kubucwebe nezinto zokuhlobisa. Yayidumile emiphakathini yasendulo, ikakhulukazi e-Egypt naseRoma, lapho kwakukholelwa ukuthi inezinto ezingokomoya nezokwelapha. Esikweni laseGibhithe, i-carnelian yayivame ukusetshenziswa eziphahleni nakwezinye izinto zokuhlobisa, futhi kwakukholelwa ukuthi inikeza isivikelo futhi ikhulise isibindi. ERoma, i-carnelian yayisetshenziswa emasongweni nakwezinye izinto zokuhloba, futhi kwakukholelwa ukuthi inamandla okudambisa izinkanuko zalowo oyifakile.

I-Carnelian yaqhubeka idumile ngeNkathi Ephakathi kanye neRenaissance, futhi yayivame ukusetshenziswa emiklamweni yobucwebe eyinkimbinkimbi, ehlotshisiwe. Namuhla, isafunwa kakhulu ngenxa yobuhle bayo nokuguquguquka kwayo. Ivamise ukusetshenziselwa imihlobiso elengayo, amacici, nezinye izinhlobo zobucwebe, futhi yaziswa ngekhono layo lokuhambisana nezinhlobonhlobo zamathoni esikhumba.

Ngaphezu kokusetshenziswa kwayo ebucwebeni, i-carnelian nayo isetshenziselwe ezinye izinjongo ezihlukahlukene emlandweni. Isetshenziswe njenge-talisman yokuvikela kanye nenhlanhla, futhi kukholakala ukuthi inamandla okuthuthukisa ukugxilisa ingqondo nenkumbulo. Ibuye isetshenziselwe ukwelapha izifo ezehlukene, okuhlanganisa ukuphazamiseka kokugaya ukudla kanye nomkhuhlane.

I-Carnelian iyiminerali enhle futhi ethakazelisayo eye yadlala indima ebalulekile emlandweni wesintu. Kusukela ekubunjweni kwayo kuya ekusetshenzisweni kwayo ebucwebeni nasezintweni zokuhlobisa, i-carnelian inesikhathi esidlule esicebile nesinezitezi. Kungakhathaliseki ukuthi uyisazi sokuma komhlaba noma unesithakazelo emadwaleni namaminerali, i-carnelian izoheha futhi ibangele uzungu.

Ukwembula I-Geology ye-Orange Calcite: Amaminerali Athakazelisayo

i-orange calcite rough

I-Orange calcite iyikristalu enhle nedumile enezindawo eziningi ezikhangayo ze-geological.

Le crystal iwuhlobo lwe-calcite, okuyiminerali ye-carbonate eyakhiwe kusukela ekuthunjweni kwe-calcium carbonate ezindaweni zasolwandle. I-Calcite iyiminerali evamile engatholakala ngemibala eminingi ehlukene, kuhlanganise nomhlophe, okwesibhakabhaka, oluhlaza okotshani, opinki, ophuzi, futhi-ke, owolintshi.

I-Orange calcite yaziwa ngombala wayo osawolintshi ogqamile, obangelwa ukuba khona kwe-iron oxide. Lo mbala ungahluka ukusuka kokuwolintshi ophaphathekile kuye kowolintshi ojulile, ocebile, kuye ngenani le-iron oxide ekhona kukristalu.

Ngaphezu kombala wayo omuhle, i-calcite ewolintshi ibuye yaziswa ngezici zayo eziningi zokwelapha. Kukholakala ukuthi inomphumela opholile futhi ophakamisayo engqondweni nasemzimbeni, futhi ivame ukusetshenziswa ekuzindleni nasekuphulukiseni ikristalu. I-Orange calcite nayo kucatshangwa ukuthi iyithuluzi elinamandla lokukhulisa ubuciko nogqozi, futhi ivamise ukusetshenziselwa ukuheha inala nokuchuma.

Ngokwesimo sezwe, i-calcite ewolintshi ingatholakala ezindaweni ezihlukahlukene emhlabeni jikelele, kuhlanganise I-united states, iMexico, neRussia. Ivame ukutholakala ngesimo samakristalu amakhulu, asobala, nakuba ingatholakala futhi kumafomu amancane, angabonakali.

Sekukonke, i-calcite ewolintshi iyikristalu enhle futhi eguquguqukayo enezindawo eziningi ezithakazelisayo ze-geological kanye nezinzuzo zokuphulukisa. Ukuthi unentshisekelo kumlando wayo we-geological, izakhiwo zokuphulukisa, or ukubukeka kwayo nje okuhle, i-calcite ewolintshi iwufanele ube nayo kunoma yimuphi umthandi wekristalu.

Ukuthola Ubuhle Obukhangayo Bamakristalu Omgogodla: Ukubheka Okujulile Kwezimo Zabo Ze-Geological

ikristalu yomgogodla

Amakristalu omgogodla awuhlobo lwamaminerali aziwa ngobuhle bawo obumangalisayo kanye nezinhlobonhlobo zemibala. Lawa makristalu angatholakala emithunzini ebomvu, ebomvana, ensomi, eluhlaza okwesibhakabhaka, eluhlaza, namnyama, futhi aziswa ngesakhiwo sawo esiyingqayizivele sekristalu nokubukeka okukhazimulayo. Kulokhu okuthunyelwe kwebhulogi, sizobheka ngokujulile izici ze-geological zamakristalu e-spinel, sihlola imvelaphi yawo, ukuqeqeshwa, kanye nezinto ezibonakalayo.

Amakristalu omgogodla ayingxenye yeqembu le-spinel lamaminerali, elihlanganisa izinhlobonhlobo ze-silicates ne-chemical formula MgAl2O4. Lawa maminerali aziwa kakhulu ukumelana nokushisa nokuguga, futhi avame ukusetshenziswa njengama-abrasives namatshe ayigugu. Amakristalu omgogodla avame ukutholakala emadwaleni e-metamorphic, njengemabula ne-serpentinite, futhi angatholakala nasemadwaleni e-metamorphosed ultramafic kanye nama-mafic igneous rocks.

Ukwakhiwa kwamakristalu e-spinel kuyinqubo eyinkimbinkimbi ehilela ukuguqulwa kwamaminerali akhona ngaphansi kwezingcindezi eziphezulu namazinga okushisa. Le nqubo, eyaziwa ngokuthi i-metamorphism, ingenzeka ngaphakathi koqweqwe lomhlaba or i-mantle, futhi ngokuvamile ihlotshaniswa nomsebenzi we-tectonic kanye nokungena kwe-magma. Njengomphumela we-metamorphism, amakristalu e-spinel angase akhe njengama-inclusions ngaphakathi kwamanye amaminerali, noma angase acwebe ngokuzimela njengamakristalu ahlukene.

Ngokuphathelene nezakhiwo zomzimba, amakristalu e-spinel ayaziwa ngamandla awo adonsela phansi aphezulu, ubulukhuni, kanye nenkomba ye-refractive. Lezi zakhiwo, kuhlanganiswe nemibala yazo egqamile nokubukeka okukhazimulayo, kwenza amakristalu e-spinel abaluleke kakhulu njengamatshe ayigugu. Eqinisweni, amakristalu e-spinel asetshenziswe njengamatshe ayigugu amakhulu eminyaka, futhi aye aziswa ngabasebukhosini nabaqoqi ngokufanayo. Amanye amakristalu omgogodla adume kakhulu emhlabeni ahlanganisa “i-Black Prince’s Ruby,” umgogodla omkhulu, obomvu obekwe ku-Imperial State Crown of England, kanye ne-“Timur Ruby,” umgogodla omkhulu, ophinki oyingxenye ye ama-Crown Jewels aseBrithani.

Sengiphetha, amakristalu e-spinel awuhlobo oluhehayo lwamaminerali aziwa ngobuhle bawo obuhehayo kanye nezici eziyingqayizivele ze-geological. Kusukela ezinhlobonhlobo zazo zemibala kuya ezintweni zazo ezibonakalayo, lawa makristalu adonse ukunaka kwezazi zokwakheka komhlaba kanye nabathandi bamatshe ayigugu ngokufanayo. Kungakhathaliseki ukuthi uyisazi sokuma komhlaba noma umane nje unokwazisa ngamagugu omhlaba, amakristalu e-spinel ngokuqinisekile azovusa uzungu futhi ajabule.

Ukuhlola i-Geology kanye nezakhiwo ze-Red Tiger Eye

I-Red tiger eye tumbel

Ihlosi elibomvu liyi-mineral ephawulekayo elaziswa ngemibala yalo eyingqayizivele namaphethini. Ivame ukusetshenziselwa ubucwebe nezinye izinto zokuhlobisa ngenxa yobuhle bayo bemvelo nokuqina. Kodwa kuthiwani ngeso lehlosi elibomvu elenza likhetheke kangaka?

Red tiger iso izinhlobonhlobo asebenza ngebhethri, i-mineral evamile etholakala ezinhlotsheni eziningi zamatshe. Ivamise ukwakhiwa ngaphakathi kwamadwala e-metamorphic, okungamatshe aguqulwe ukushisa nokucindezela. Uma i-quartz ingaphansi kwalezi zimo, ingathatha izakhiwo nemibala emisha, okuholela kumaminerali afana ne-red tiger eye.

Ihlo lehlosi elibomvu lithola umbala walo ohlukile ku-iron oxide, ekhona kumaminerali ngamanani amancane. Lapho i-iron oxide ichayeka ekukhanyeni, ibuyisela emuva amaza abomvu, okwenza iso lengwe elibomvu libe nombala walo obomvu. Umbala wehlo lehlosi elibomvu ungasuka kobomvana ophaphathekile uye kobomvu ngokujulile, kuye ngenani le-iron oxide elikhona.

Ngaphezu kombala walo, iso lengwe elibomvu liyaziwa ngokuxoxa, or ikhono lokubonisa ukukhanya ebhandeni elincane. Lokhu kunikeza i-mineral umphumela “weso lekati”, yingakho ngokuvamile ibizwa ngokuthi iso lengwe. I-chatoyancy yehlo lehlosi elibomvu ibangelwa ukuhlelwa kwemicu ngaphakathi kweminerali, ebonisa ukukhanya ngendlela ethile.

Ihlo lehlosi elibomvu linemisebenzi eminingi engokoqobo ngaphezu kwenani lalo lokuhlobisa. Kuyiminerali eqinile uma kuqhathaniswa, okwenza ifanelekele ukusetshenziswa ebucwebeni nakwezinye izinto ezingase ziguge. Ihlo lehlosi elibomvu kukholakala ukuthi linezinto zokuphulukisa futhi livame ukusetshenziswa emithini yendabuko kanye nemikhuba yomoya.

Sengiphetha, iso lengwe elibomvu liyiminerali ethakazelisayo elaziswa ngombala walo oyingqayizivele namaphethini. Yakho ukuqeqeshwa ngaphakathi kwamadwala e-metamorphic kanye nokuba khona kwe-iron oxide kuyinikeza isici sayo sombala obomvu nokuxoxa. Kungakhathaliseki ukuthi ungumthandi wokwakheka komhlaba noma umane ujabulela ubuhle bamaminerali, iso lengwe elibomvu liyiminerali ekhangayo futhi ehlukahlukene okufanele ihlolwe.