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Bilder zu 'Panthalassa' gefunden, 6

Earth 443 million years ago - Artist View - Silurian Earth - This is how the Earth may have appeared 443 million years ago during the Silurian period. The northern most continent is what would become today's Siberia and to the west of that is the Panthalassic Ocean. South of the equator to the east is the early - Palaeozoic continent of Baltica later to form part of Eurasia, while to the east is the continent of Laurentia later to become the core of North America. Further south is the Rheic Ocean and to the west the Iapetus Ocean

Earth 443 million years ago - Artist View - Silurian Earth - This is how the Earth may have appeared 443 million years ago during the Silurian period. The northern most continent is what would become today's Siberia and to the west of that is the Panthalassic Ocean. South of the equator to the east is the early - Palaeozoic continent of Baltica later to form part of Eurasia, while to the east is the continent of Laurentia later to become the core of North America. Further south is the Rheic Ocean and to the west the Iapetus Ocean

Walter B Myers

PIX4633402

The Earth 600 million years ago - Artist's view - Ediacaran Earth - The Earth seen about 600 million years ago after an important period of glaciation. This is how the Earth may have appeared 600 million years ago following the Cryogenian “” Snowball Earth”” period. The worldwide glaciers have melted and the ocean is largely liquid again. During this, the Ediacaran period, it is hypothesized that all of the Earth's landmasses had merged into a single supercontinent known as Pannotia, also known as the Vendian supercontinent. Surrounding this massive landmass is the vast Panthalassic Ocean, also known as Panthalassa. While the ocean was home to a variety of evolving multicellular life forms including the ubiquitous Dickinsonia costata, it is not believed that life had moved to dry land with possible exception of bacteria and other microbial colonies

The Earth 600 million years ago - Artist's view - Ediacaran Earth - The Earth seen about 600 million years ago after an important period of glaciation. This is how the Earth may have appeared 600 million years ago following the Cryogenian “” Snowball Earth”” period. The worldwide glaciers have melted and the ocean is largely liquid again. During this, the Ediacaran period, it is hypothesized that all of the Earth's landmasses had merged into a single supercontinent known as Pannotia, also known as the Vendian supercontinent. Surrounding this massive landmass is the vast Panthalassic Ocean, also known as Panthalassa. While the ocean was home to a variety of evolving multicellular life forms including the ubiquitous Dickinsonia costata, it is not believed that life had moved to dry land with possible exception of bacteria and other microbial colonies

Walter B Myers

PIX4633308

Shonisaure - Shonisaurus - A 30-ton Shonisaurus (Shonisaurus) about to devour some belemnites.

Shonisaure - Shonisaurus - A 30-ton Shonisaurus (Shonisaurus) about to devour some belemnites.

Walter B Myers

PIX4662169

A ring of rocks and dust is orbiting the Earth. The massive continent below is Pangee and the ocean to the west is Panthalassa. This is what Earth was supposed to look like at the end of Permian, about 260 million years ago, before the first dinosaurs appeared. This ring around the Earth was of earthly origin, constitutes debris thrown into orbit by collision with a meteorite or comet. Over time, these debris have fallen or fallen to Earth in a meteorite rain - A dusty ring arc orbits four thousand miles above Earth's equator. The massive continent below is Pangea and the ocean to the west is Panthalassa. This is how the Earth may have appeared during the end of the Permian period, a time just prior to the appearance of the dinosaurs, when continental drift was pulling Pangea apart into the seven continents we know today - 260 million years ago the Earth may have been host to ring arcs similar to the incomplete rings that currently circumscribe the planet Neptune . Unlike Neptune's rin

A ring of rocks and dust is orbiting the Earth. The massive continent below is Pangee and the ocean to the west is Panthalassa. This is what Earth was supposed to look like at the end of Permian, about 260 million years ago, before the first dinosaurs appeared. This ring around the Earth was of earthly origin, constitutes debris thrown into orbit by collision with a meteorite or comet. Over time, these debris have fallen or fallen to Earth in a meteorite rain - A dusty ring arc orbits four thousand miles above Earth's equator. The massive continent below is Pangea and the ocean to the west is Panthalassa. This is how the Earth may have appeared during the end of the Permian period, a time just prior to the appearance of the dinosaurs, when continental drift was pulling Pangea apart into the seven continents we know today - 260 million years ago the Earth may have been host to ring arcs similar to the incomplete rings that currently circumscribe the planet Neptune . Unlike Neptune's rin

Walter B Myers

PIX4669572

Earth at the end of Permian - Ring arcs over the Permian Earth - A ring of rocks and dust is orbiting the Earth. The massive continent below is Pangee and the ocean to the west is Panthalassa. This is what Earth was supposed to look like at the end of Permian, about 260 million years ago, before the first dinosaurs appeared. This ring around the Earth was of earthly origin, constitutes debris thrown into orbit by collision with a meteorite or comet. Over time, these debris have either fallen or fallen back to Earth in a meteorite rain. A dusty ring arc orbits four thousand miles above Earth's equator. The massive continent below is Pangea and the ocean to the west is Panthalassa. This is how the Earth may have appeared during the end of the Permian period, a time just prior to the appearance of the dinosaurs, when continental drift was pulling Pangea apart into the seven continents we know today. 260 million years ago the Earth may have been host to ring arcs similar to the incomplete

Earth at the end of Permian - Ring arcs over the Permian Earth - A ring of rocks and dust is orbiting the Earth. The massive continent below is Pangee and the ocean to the west is Panthalassa. This is what Earth was supposed to look like at the end of Permian, about 260 million years ago, before the first dinosaurs appeared. This ring around the Earth was of earthly origin, constitutes debris thrown into orbit by collision with a meteorite or comet. Over time, these debris have either fallen or fallen back to Earth in a meteorite rain. A dusty ring arc orbits four thousand miles above Earth's equator. The massive continent below is Pangea and the ocean to the west is Panthalassa. This is how the Earth may have appeared during the end of the Permian period, a time just prior to the appearance of the dinosaurs, when continental drift was pulling Pangea apart into the seven continents we know today. 260 million years ago the Earth may have been host to ring arcs similar to the incomplete

Walter B Myers

PIX4633164

Earth 200 million years ago - Artist's view - Early Jurassic Earth - Earth seen at the beginning of the Jurassic, about 200 million years ago. The western hemisphere is representative, the north is up. The Pangee has just split, forming Laurasia to the north and Gondwana to the south. This is how the western hemisphere of the Earth may have appeared 200 million years ago during the Early Jurassic period. North is at the top. During this period continental drift, driven by the massive forces of plate tectonics, had just begun to break the supercontinent of Pangea into Laurasia in the north and Gondwana in the south. In this image the nascent North American continent has just broken away from North Africa while South America and the rest of Africa remain joined as Gondwana. To the west in the global Panthalassa ocean are strips of land corresponding to the Wrangellia Terrane which later merged with western North America

Earth 200 million years ago - Artist's view - Early Jurassic Earth - Earth seen at the beginning of the Jurassic, about 200 million years ago. The western hemisphere is representative, the north is up. The Pangee has just split, forming Laurasia to the north and Gondwana to the south. This is how the western hemisphere of the Earth may have appeared 200 million years ago during the Early Jurassic period. North is at the top. During this period continental drift, driven by the massive forces of plate tectonics, had just begun to break the supercontinent of Pangea into Laurasia in the north and Gondwana in the south. In this image the nascent North American continent has just broken away from North Africa while South America and the rest of Africa remain joined as Gondwana. To the west in the global Panthalassa ocean are strips of land corresponding to the Wrangellia Terrane which later merged with western North America

Walter B Myers

PIX4633329

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