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Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

officialfabletown: nubbsgalore: striped icebergs form as meltwater refreezes in crevasses atop glaciers before air bubbles can become trapped in the ice later calved into icebergs, or when supercooled seawater freezes inside cracks beneath an ice shelf,

officialfabletown: nubbsgalore: striped icebergs form as meltwater refreezes in crevasses atop glaciers before air bubbles can become trapped in the ice later calved into icebergs, or when supercooled seawater freezes inside cracks beneath an ice shelf,

cameoappearance: nubbsgalore: striped icebergs form as meltwater refreezes in crevasses atop glaciers before air bubbles can become trapped in the ice later calved into icebergs, or when supercooled seawater freezes inside cracks beneath an ice shelf,

cameoappearance: nubbsgalore: striped icebergs form as meltwater refreezes in crevasses atop glaciers before air bubbles can become trapped in the ice later calved into icebergs, or when supercooled seawater freezes inside cracks beneath an ice shelf,

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

nubbsgalore: striped icebergs form as meltwater refreezes in crevasses atop glaciers before air bubbles can become trapped in the ice, which is later calved into icebergs, or when supercooled seawater freezes inside cracks beneath an ice shelf, which

nubbsgalore: striped icebergs form as meltwater refreezes in crevasses atop glaciers before air bubbles can become trapped in the ice, which is later calved into icebergs, or when supercooled seawater freezes inside cracks beneath an ice shelf, which

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

nubbsgalore: striped icebergs form as meltwater refreezes in crevasses atop glaciers before air bubbles can become trapped in the ice, which is later calved into icebergs, or when supercooled seawater freezes inside cracks beneath an ice shelf, which

nubbsgalore: striped icebergs form as meltwater refreezes in crevasses atop glaciers before air bubbles can become trapped in the ice, which is later calved into icebergs, or when supercooled seawater freezes inside cracks beneath an ice shelf, which

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

Jade and striped icebergs. “When seawater at depths of more than 1,200 feet freezes to the underside of massive ice shelves like East Antarctica’s Amery Ice Shelf, it forms ‘marine ice.’ Enormous hunks of ice calve—or break off—from the ice

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