VIRTUAL GEOLOGIC TIME SCALE
The Geologic Time Scale is a system of chronological dating. It is used by geologists, paleontologists, and other Earth scientists to describe the timing and relationships of events in geologic history. It was developed through the study and observation of layers of rock and relationships as well as the times when different organisms appeared, evolved and became extinct. This Virtual Geologic Time Scale was built by 3rd grade students at The Cottonwood School of Civics and Sciences in Portland, Oregon. This project is by kids, and for kids (of all ages)!
Click on the Period names below to read, view, and hear more!
Nobody has written about this period. Email us at info@ricenorthwestmuseum if you have something you’d like to add!
The Cretaceous period occurred between 145.5 and 65.5 million years ago. About 65.5 million years ago a big meteor hit Earth. Even the dinosaur Gallimimus could not outrun the tsunami created by the meteor. And the Gallimimus can go like 20 miles per hour! Even if some dinosaurs survived all of the volcanoes and all of that they would have starved to death.
The T-Rex is not the biggest dinosaur. The largest carnivorous dinosaur was Spinosaurus. The next biggest dinosaur is Giganotosaurus, a little bigger than the Yangchuanosaurus.
If you thought that all herbivores were the prey of carnivores then you are wrong. There are some herbivores large enough to kill carnivores. During the Cretaceous period ferns grew all over the jungle floor. If you had a cut you would want to rub it under a fern. A fern is like medicine isn’t that cool?
201 million-145 million years ago, the Jurassic period was really cool. It had a lot of dinosaurs. It had a wet climate and lots of plants. The seas were high.
During the Jurassic period Earth’s climate changed from hot and dry to warm and humid. Most of the plants were tree ferns. At the start of the period Pangea continued to break up. On land dinosaurs were making their mark in a big way. Some dinosaurs are 85 feet long (that’s 26 meters). The Jurassic Period took place 201 to 145 million years ago.
The Triassic era started 251 million years ago, and ended 201 million years ago. In the Triassic era little shrew-like creatures evolved. They were called Morganucodontids. These were the first mammals. They appeared at the end of the Triassic era.
The Triassic era is important because it is when the dinosaurs first evolved! The Chindesaurus, Coelophysis, Coloradisaurus, and the Eoraptor were some of the first dinosaurs.
Pterosaurs were flying reptiles that lived in the Triassic era. Also in the Triassic era reef coral, fish and insects evolved. The Triassic era is important because it is when a lot of the creatures evolved.
—by Marlow L. Batzler
The Triassic period had a major depopulation in the oceans because of the high carbon dioxide levels. Event 1: The Triassic period followed the great mass extinction. Event 2: Plants and iInsects did not go through any extensive evolutionary advances during the Triassic. Event 3: The sea was similar to present day or slightly higher. Event 4: Due to the dry climate, the interior of Ppangaea was mostly desert. Event 5: The first mammals evolved near the end of the Triassic period from the nearly extinct Therapsids.
—by Georgia Abby
In this period there are lots of events. One interesting fact is that Permian got its name from the Perm region in Russia.
Also the Permian ended with the biggest extinction in the world! The Pemian was 298.9 million years ago. The Pangea supercontinent was shaped like the letter “c”. Synapsid’s skulls had a hole.
Plants sometimes had spores, and sometimes had seeds. Seed-bearing plants called Gymnosperms were widespread.
In the Carboniferous period new plants developed in the warm humid climate and new mountains formed. The Carboniferous period was in the Paleozoic era, 400 million years to 299 million years ago. In the middle and end of the Carboniferous period the land was rising out of the water. This caused the shallow seas to become swamps between the ocean and dry land. Animals such as early amphibians were born in the water and then later moved on to land. The plants in the Carboniferous period were ferns and lycopods.
These plants produced so much oxygen that they grew to huge sizes. It was the age of oxygen! The end of the Carboniferous was marked by global climate changes and glaciers that covered the South Pole.
—by Evie june
The Silurian Period occurred 443 to 416 million years ago. It was the third period in the Paleozoic era. It followed the Ordovician period and preceded the Devonian period. During this time continental landmasses were low and sea levels started rising. Silurian fossils show evidence of extensive reef building and the first signs of life beginning to colonize the new estuary, freshwater and terrestrial ecosystems. A warm stable climate provided for one of the most significant developments of the Paleozoic era to take place during the Silurian period: the arrival of the first plants to colonize the land.
—by Harlow Landau
By Noah Mathis
The Ordovician Era time was between 490 and 443 million years ago. One type of animal that lived during this period was the horseshoe crab. They are still here today! Some other living things were reefs and primitive plants. There were even more plants like mosses and bryophytes. It had a 20 million year ice age and 2nd biggest mass extinction ever. There were even glaciers that formed over Africa. After the mass extinction, about nine of every ten plant and animal species on the planet were gone. Then there was a wipe out of half of all the sea animals. Then there were freezing conditions towards the end of the Ordovician.
—by Noah Mathis
In the Ordovician there was lots of life– animals, plants, trilobites–lots of life. There were a few volcanoes. Then the earth was a big ice ball. One theory about how it happened was that there was a star that died. Gamma rays damaged the Earth’s atmosphere, making the earth freeze up. Then our sun’s ultraviolet light harmed life on Earth. 85% of life died which was a bad time for the trilobites. Only 15% of life was left.
What life was in the Ordovician: a list of animals and plants!
1. trilobite animal.
2. cryptospores plant.
3. Brachiopod animal.
4. mollusca animal.
5. crinoids animal.
6. green algae plant.
7. moss plant.
8. liverworts plant.
—by Graham Pliska
The Cambrian Period is the first geological period of the Paleozoic era that produced the most powerful eruption of evolution. The Cambrian Period started 541 million years ago. Life on Earth changed greatly during this period. This period lasted for about 53 million years. The period gets its name from Cambria, the Roman name for Wales. During the Cambrian period, some organisms used carbonate minerals for shells, so they had hard parts which could become fossils. There were many different kinds of life during the Cambrian period. In the beginning of this period the Cambrian explosion occurred. This adaptive radiation produced the first members of the main groups of animals, or phyla. Almost all of this new life was in the oceans. In the early Cambrian years species such as the archaeocyathids (sponge like animals) built the first carbonate reefs. There was little life on land except a layer of microbes which were microorganisms- that is, organisms which are microscopic, meaning so small that people cannot see them with the naked eye.
In the Cambrian period a lot of animals evolved!The Cambrian period lasted 53 million years. Most animals were a lot like insects. Almost no life existed when the Cambrian period started. The largest predator was a shrimp-like animal called Anomalocaris. Haikouichythes was an early jawless fish. Many things evolved during the Cambrian period. It was cold when the Cambrian period started but got warmer. Glaciers melted in the Cambrian period. Microscopic worms lived at the bottom of the ocean. Many fossils have been found from the Cambrian period.
PRECAMBRIAN TIME PERIOD
The Precambrian period is 80% of Earth’s past. It started 4.5 billion years ago. It is made up of the Archean and Proterozoic eons. There were a lot of changes in the Precambrian. At this time, molten lava made land masses and the ozone layer was created. Oceans were created from water vapor in the atmosphere. Life started in the oceans. Geologists have found bacteria micro fossils in sedimentary rock from the Precambrian. The first multi-celled organisms were from this time period. Minerals we use today can be found in the Precambrian like silver, iron, nickel, and copper.
—by Miles Williams