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Pytheas also spoke of the waters around Thule and of those places where land properly speaking no longer exists, nor sea nor air, but a mixture of these things, like a "marine lung", in which it was said that earth and water and all things are in suspension as if this something was a link between all these elements, on which one can neither ...
The Greek explorer Pytheas of the Greek city of Massalia (now Marseille, France) is the first to have written of Thule, after his travels between 330 and 320 BC.Pytheas mentioned going to Thule in his now lost work, On The Ocean Τὰ περὶ τοῦ Ὠκεανοῦ (ta peri tou Okeanou).
Pythia's Oasis is a cold seep on the ocean floor 50 miles (80 km) off the coast of Newport, Oregon, United States (1], characterized by a focused stream of highly altered fluid that is approximately 9 °C (16 °F) above normal ocean background temperature. Early results indicate "elevated flow rates" sustained for about 1,500 years.
In the Faroe Islands, wild, unpredictable weather — fierce winds and rain, and thick fog that settles like a curtain — can sometimes make travel by car or ferry problematic.
Surrounded by the vast Pacific Ocean, Japan’s Ise-Shima region is a place where ancient traditions, spirituality and the great outdoors collide. ‘Sea women’ and sacred waterfalls: Exploring ...
1. Add to Grains. Turn yesterday’s soup into today’s healthy bowl. Start with a base of grains like rice, farro, or quinoa. Add roasted veggies and a protein.
Oblique view from Apollo 15, facing south Close up of the south wall of Pytheas crater from Apollo 17. Pytheas is a small lunar impact crater located on the southern part of the Mare Imbrium, to the south of the crater Lambert. It was named after ancient Greek navigator and geographer Pytheas of Massalia. [1]
In part, Sarmast [7] bases his theory that Atlantis can be found offshore of Cyprus beneath 0.9 mile (1.5 km) of water on an abundance of evidence that the Mediterranean Sea dried up during the Messinian Salinity Crisis when its level dropped by 2 to 3 miles (3.2 to 4.9 km) below the level of the Atlantic Ocean as the result of tectonic uplift ...
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