@tali.alanaa: always freaking smiling

tali alana 🫧

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Friday 06 November 2026 22:00:40 GMT

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⃟ :

Ugly too

2026-11-06 22:34:51

0

kenn 💕 :

Can i put the smiley picture of u from td

2026-11-06 22:19:55

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gigi :

ur so cute

2026-11-06 22:36:34

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nanicakes :

just jolly

2026-11-06 22:11:26

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amanda :

the cutest smile

2026-11-06 23:48:06

0

️ :

my smiley princess 💗

2026-11-06 22:02:42

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Janae❦ :

cutie

2026-11-06 22:06:44

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gtm.jaz𓅓 :

2026-11-06 22:35:46

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Other Videos

Why does pegmatite have such HUGE crystals? Pegmatite is an extremely coarse-grained igneous rock that usually forms during the final stages of magma crystallisation, commonly around granitic intrusions. As a body of magma cools underground, minerals begin to crystallise — but not everything fits neatly into those early-forming crystals. Water and other volatile components become concentrated in the remaining melt, along with elements that don’t easily fit into the crystal structures of the common minerals. This leftover melt becomes increasingly water-rich and chemically concentrated. Water helps ions move more easily through the melt, allowing crystals to grow incredibly quickly and, crucially, VERY large. 🤯 That’s why pegmatites can contain spectacular crystals of quartz, feldspar and mica that are centimetres — and sometimes even metres — across. But pegmatites can also concentrate less common elements such as lithium, beryllium, boron, tantalum and rare earth elements, which is why they’re so interesting when we’re exploring for critical minerals. Essentially, pegmatite is what happens when you get down to the last, volatile-rich leftovers of a crystallising magma body… …and those leftovers can create some absolutely spectacular rocks. 🪨✨ #ScottishGeologist #Geology #Scottishgeology

Why does pegmatite have such HUGE crystals? Pegmatite is an extremely coarse-grained igneous rock that usually forms during the final stages of magma crystallisation, commonly around granitic intrusions. As a body of magma cools underground, minerals begin to crystallise — but not everything fits neatly into those early-forming crystals. Water and other volatile components become concentrated in the remaining melt, along with elements that don’t easily fit into the crystal structures of the common minerals. This leftover melt becomes increasingly water-rich and chemically concentrated. Water helps ions move more easily through the melt, allowing crystals to grow incredibly quickly and, crucially, VERY large. 🤯 That’s why pegmatites can contain spectacular crystals of quartz, feldspar and mica that are centimetres — and sometimes even metres — across. But pegmatites can also concentrate less common elements such as lithium, beryllium, boron, tantalum and rare earth elements, which is why they’re so interesting when we’re exploring for critical minerals. Essentially, pegmatite is what happens when you get down to the last, volatile-rich leftovers of a crystallising magma body… …and those leftovers can create some absolutely spectacular rocks. 🪨✨ #ScottishGeologist #Geology #Scottishgeology

#casa #Home

Lots of adrenaline last night… #wrestling #wrestler #collegewrestling

Lots of adrenaline last night… #wrestling #wrestler #collegewrestling

تلاوة عطرة لسورة الكهف #تلاوة_خاشعة #creatorsearchinsights #اكسبلور #amazing #4u

تلاوة عطرة لسورة الكهف #تلاوة_خاشعة #creatorsearchinsights #اكسبلور #amazing #4u

Mua nồi cho gia đình thì các bác phải chú ý nhé #xuhuong #tikhub #noiapsuat #noiapsuatdanang #noiapsuatdien

Mua nồi cho gia đình thì các bác phải chú ý nhé #xuhuong #tikhub #noiapsuat #noiapsuatdanang #noiapsuatdien

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