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Поставио: maja | Категорија: Лесни профил Капела у Батајници, НВО "Еколошки покрет Земун", Новости, акције | Коментара: 0 | Датум: 30. октобар, 2019 |

UNDER CONSTRUCTION!!!

HOW WAS THE LOESS PROFILE KAPELA IN BATAJNICA FORMED?

LOESS IS A DEPOSIT OF DUST AND FINE SAND BLOWN BY WINDS OR BROUGHT BY RIVERS TO GRASSY PLAINS DURING THE ICE AGE.

THE KAPELA PROFILE DURING THE LAST 800,000 YEARS.  

If we had a mill large enough to grind the Alps and add a little powder from the Carpathians, we would get the same sediment as it is found in the loess profiles of Batajnica area. This material was brought by rivers from the mountains, and then it was carried by the wind across the steppe plains in the vicinity of the Kapela.

Two layers of volcanic ash have been observed within the Kapela profile, which talk about turbulent, often catastrophic, natural processes – volcanic eruptions. The volcanic material is about 140,000 and 480,000 years old, and it originates from the eruptions on the Apennine Peninsula.

MILUTIN MILANKOVIĆ

THIS GREAT SCIENTIST CALCULATED THE OCCURRENCE PERIODS AND THE DURATION OF ICE AGES, WHICH WAS FULLY CONFIRMED BY THE RESEARCH OF LOESS LAYERS

THE KAPELA PROFILE DURING THE LAST 800,000 YEARS


AND THE VOLCANIC  ASH FROM ITALY BROUGHT TO THE PANNONIAN PLAIN BY WIND

INHABITANTS: STEPPE ELEPHANT, WOOLLY MAMMOTH, WOOLLY RHINO, GIANT DEER, MOOSE, CAVE LION, CAVE BEAR

LOESS DOLLS WERE CREATED BY THE DEPOSITION OF LIMESTONE IN LOESS AND THEY ARE REAL SCULPTURES OF UNUSUAL SHAPES

THE KAPELA LOESS PROFILE IN BATAJNICA

FROM THE ALPS ROCK MATERIAL CRUSHED WITH GLACIAL EROSION WAS DISPERSED BY THE RIVERS AND WIND… TO THE PANONIAN PLAIN AND BATAJNICA WHERE IT WAS DEPOSITED

DEPOSITED MATERIAL:

DARKER SEDIMENTS

PERIOD BETWEEN ICE AGES

VOLCANIC  ASH

PERIOD OF VOLCANIC ERUPTIONS

LIGHTER SEDIMENTS

PERIOD OF ICE AGES


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