Question

✤ Blood river Antarctica
✤ Avokigahara forest
✤ Krishna butter ball stone

I need some interesting facts ..!! so don't simply copy from Google and paste ....

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Answer 1

Answer :

☆ Blood Falls is an outflow of an iron oxide-tainted plume of saltwater, flowing from the tongue of Taylor Glacier onto the ice-covered surface of West Lake Bonney in the Taylor Valley of the McMurdo Dry Valleys in Victoria Land, East Antarctica

☆ Aokigahara (青木ヶ原), also known as the Sea of Trees (樹海, Jukai), is a forest on the northwestern flank of Japan's Mount Fuji, thriving on 30 square kilometres (12 sq mi) of hardened lava laid down by the last major eruption of Mount Fuji in 864 CE.[1] The western edge of Aokigahara, where there are several caves that fill with ice in winter, is a popular destination for tourists and school trips. Parts of Aokigahara are very dense, and the porous lava absorbs sound, helping to provide visitors with a sense of solitude.

☆ Krishna's Butterball (also known as Vaan Irai Kal[1] and Krishna's Gigantic Butterball) is a gigantic granite boulder resting on a short incline in the historical coastal resort town of Mamallapuram in Tamil Nadu state of India.

Since it is part of the Group of Monuments at Mamallapuram, a UNESCO World Heritage Site built during 7th- and 8th-century CE as Hindu religious monuments by the Pallava dynasty, it is a popular tourist attraction.[3][4][5] It is listed as a protected national monument by the Archeological Survey of India. thank you please follow me ya

Answer 2

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Blood Falls is an outflow of an iron oxide-tainted plume of saltwater, flowing from the tongue of Taylor Glacier onto the ice-covered surface of West Lake Bonney in the Taylor Valley of the McMurdo Dry Valleys in Victoria Land, East Antarctica.

Iron-rich hypersaline water sporadically emerges from small fissures in the ice cascades. The saltwater source is a subglacial pool of unknown size overlain by about 400 metres (1,300 ft) of ice several kilometers from its tiny outlet at Blood Falls.

The reddish deposit was found in 1911 by the Australian geologist Griffith Taylor, who first explored the valley that bears his name.[1] The Antarctica pioneers first attributed the red color to red algae, but later it was proven to be due to iron oxides.

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