The arrival of European settlers and traders led to the displacement of indigenous peoples from their traditional territories, disrupting their trade networks and introducing new diseases.
Rock formations
Deposited in layers from the oldest to the youngest on the bottom
Paleontologists
Scientists who study early life forms from animal and plant fossils
The Burgess Shale Fossil Beds have preserved the soft tissue of many species, allowing scientists to study these specimens in detail
Fossils look much the same as they did a half billion years ago
Geologic time intervals
Precambrian Era: 4600 to 600 millions of years ago
Paleozoic Era
Mesozoic Era: 225 to 65 millions of years ago
Cenozoic Era: 65 millions of years ago to present day
All that science knows about the ancient past, it has learned from rock and fossil records
Scientists estimate that Earth is about 4.6 billion years old
The first simple organisms and first soft-bodied animals appeared during the Precambrian Era
The first reptiles, large land animals, insects, large land plants and fish with jaws appeared during the Paleozoic Era
Dinosaurs ruled and became extinct during the Mesozoic Era. The first flowering plants, birds and mammals appeared
In the Cenozoic Era was the appearance of most modern species, many more species of mammals, first grasses, and first human-like species (about 2-3 millions of years ago)
Chemical weathering
Acid rain
Soda spilled on the road
Biological weathering
Plants growing through cement
Animals burrowing tunnels in the ground
Sediment
Silt, sand, mud, and gravel carried by flowing rivers
Deposition
Process of sediments being deposited on surface features
Landforms created by running water
Sudden and fast movements of rocks and soil down a slope
Moving masses of ice and snow
Bedrock
Layer of solid rock beneath the loose rock fragments
Minerals
Pure, naturally occurring solid materials that are the building blocks of rock
Properties of minerals
Color
Luster
Streak
Cleavage and fracture
Mohs hardness
Color alone is not enough to identify a mineral</b>
Igneous rocks
Rocks that form from hot, molten rock
Igneous rocks
Obsidian
Pumice
Pegmatite
Basalt
Intrusive igneous rock
Igneous rock formed from magma that cooled and hardened beneath the surface
Extrusive igneous rock
Igneous rock that was formed from lava cooling on Earth's surface
Sedimentary rocks
Layers of rock that form when small pieces of rock are carried by water or wind and settle or sink down in water onto the rocks below them
Sedimentary rocks
Limestone
Shale
Conglomerate
Sandstone
Metamorphic rocks
Rocks that have been changed because of intense pressure and heat within Earth's interior
Metamorphic rocks
Gneiss
Marble
Schist
Quartzite
Slate
Rock cycle
Process by which rock is changed from one class to another
The Precambrian rock formation underlies all of Alberta, though it is only exposed in the northeast corner of the province. It is made up of igneus and metamorphic rocks
The Interior Plain of Alberta, Saskatchewan and Manitoba is made up of various layers of sedimentary rock that are between 544 million and 65 million years old
Continental drift
Alfred Wegener's hypothesis, now accepted, of the movement of continental land masses
At one time all continents were joined together in a single land mass, called Pangaea
Wegener noticed that several fossils of similar plants and animals had been found on different continents
Wegener discovered the geology had found the same kind of rocks on both sides of the Atlantic Ocean, and the mountain range that ran through Britain and Norway matched the Appalachians in eastern North America
The fossils of Glossopteris plants, which were ferns, could not have travelled across the ocean
The folded, tilted or vertically oriented sedimentary rock layers show that glaciers once covered this land
The ancient tropical forests produced the coal deposits which seem to have once been connected
Plate tectonics
The idea that the continental crust is broken up into large areas called plates, all plates are moving very slowly in various directions