1.Igneous 1.Igneous - formed when molten rock cools. 2.Sedimentary 2.Sedimentary – formed by the “cementing together” of small grains of sediment. 3.Metamorphic 3.Metamorphic – rocks changed by the effect of heat and pressure.

These are rocks formed by the cooling of molten rock (magma.) magma volcano Magma cools and solidifies forming igneous rocks

When molten rock cools, forming what are called igneous rocks, radioactive atoms are trapped inside. Afterwards, they decay at a predictable rate. By measuring the quantity of unstable atoms left in a rock and comparing it to the quantity of stable daughter atoms in the rock, scientists can estimate the amount of time that has passed since that rock formed. Absolute geologic dating and relative geologic dating are two methods by which scientists try to determine the age of geologic evidence. Carbon-14 dating is an example of absolute dating, and the law of superposition is an example of relative dating.

Sedimentary Rocks are rocks formed when particles of sediment build up and are “cemented together” by the effect of pressure and minerals. sea Fragments washed to the sea Sedimentary rocks Rocks are broken up by the action of weather Getting older

Sedimentary rock makes up about 75% of the rocks on the Earth’s surface. Sedimentary rocks form on the surface of the Earth, anywhere that sand, mud, or other types of sediment collect. Sedimentary rock layers can be disturbed by igneous rock. This happens when molten rock forces it way up through the layers above it. This forms igneous rock sections within and across the sedimentary layers. The sedimentary rock layers must be there first, therefore the igneous rock intrusions are younger than the layers it cuts through. Sometime the molten rock will force its way to the surface and erupt, creating a younger igneous layer at the surface. With time, more sedimentary layers can form on top of the igneous rock. Igneous rock is always younger than rock layers it cuts through.

Metamorphic rocks are formed by the effect of heat and pressure on existing rocks. This can greatly affect the hardness, texture or layer patterns of the rocks. Magma metamorphic rock forming here heat Pressure from surface rocks

Faults are fractures in Earth's crust where rocks on either side of the crack have slid past each other. There are three kinds of faults: strike-slip, normal and reverse faults. Each type is the outcome of different forces pushing or pulling on the crust, causing rocks to slide up, down or past each other.

indicate rocks are sliding past each other, with little to no vertical movement. Both the San Andreas and Anatolian Faults are strike-slip.

Normal faults: create space. Two blocks of crust pull apart, extending the crust. –The Basin and Range Province in North America and the East African Rift Zone are two well-known regions where normal faults are spreading apart Earth's crust.

Reverse faults: also called thrust faults, squeeze the crust, pushing two blocks of crust on top of each other. –These faults are commonly found in mountain ranges such as the Himalayas and the Rocky Mountains.

Cylinders of ice that are drilled out of glaciers and polar ice sheets that help scientists know more about past climates. When snow falls it carries with it the compounds that are in the air at the time. In areas where temperatures are rarely above freezing (ice sheets and glacial areas), this builds up layer upon layer of compacted snow which becomes ice. Within these ice layers there is a record of the atmosphere at the time that the snow creating the ice layers fell.

Formed about 260 million years ago during the Permian Period. Earth’s continents moved together to form a great landmass, or supercontinent. –This caused deserts to expand to the tropics and sheets of ice covered land closer to the South Pole. –Many organisms could not survive the new climates.

Pangea holds together for much of the Triassic period where hot, dry conditions dominate the center of Pangea. Pangea broke apart during the Jurassic period as North America separated from Africa and South America.

Fossils

How do fossils form? Fossils are the preserved remains or traces of living things. Fossils are the preserved remains or traces of living things. –Fossils provide evidence of how life has changed over time. –Fossils also help scientists infer how Earth’s surface has changed. –Fossils are clues to what past environments were like.

How do fossils form? Most fossils form when living things die and are buried by sediments. The sediments slowly harden into rock and preserve the shapes of the organisms. Most fossils form when living things die and are buried by sediments. The sediments slowly harden into rock and preserve the shapes of the organisms.

How do fossils form? Scientists who study fossils are called paleontologists. Scientists who study fossils are called paleontologists.

How do fossils form? Fossils are usually found in sedimentary rock. Fossils are usually found in sedimentary rock. Sedimentary rock is the type of rock that is made of hardened sediment. Sedimentary rock is the type of rock that is made of hardened sediment.

What are the different kinds of fossils? Fossils found in rock include petrified fossils, molds and casts, carbon films, and trace fossils. Fossils found in rock include petrified fossils, molds and casts, carbon films, and trace fossils. Other fossils form when the remains of organisms are preserved in substances such as tar, amber, or ice. Other fossils form when the remains of organisms are preserved in substances such as tar, amber, or ice.

What are the different kinds of fossils? Petrified Fossils Petrified Fossils –A fossil may form when the remains of an organism become petrified. –Petrified means “turning to stone” –Petrified fossils are fossils in which minerals replace all or part of an organism.

What are the different kinds of fossils? Molds and casts Molds and casts –A mold is a hollow area in sediment in the shape of an organism or part of an organism. A mold forms when the hard part of the organism such as a shell, is buried in sediment. A mold forms when the hard part of the organism such as a shell, is buried in sediment. –A cast is a copy of the shape of an organism. Water carrying dissolved minerals and sediment may seep into the empty space of a mold. If the water deposits the minerals and sediment there, the result is a cast. Water carrying dissolved minerals and sediment may seep into the empty space of a mold. If the water deposits the minerals and sediment there, the result is a cast.

Molds and Casts

What are the different kinds of fossils? Carbon films Carbon films –An extremely thin coating of carbon on rock. HOW DOES A CARBON FILM FORM? –When sediment buries an organism, some of the materials that make up the organism can become gases. These gases escape from the sediment, leaving carbon behind. Eventually, only a thin film of carbon remains.

Carbon Films

What are the different kinds of fossils? Trace fossils Trace fossils –Trace fossils provide evidence of the activities of ancient organisms. –A fossilized footprint is on example of a trace fossil. –Other examples of trace fossils include the trails that animals followed or the burrows that they lived in.

Trace Fossils

What are the different kinds of fossils? Preserved Remains Preserved Remains –Some processes preserve the remains of organisms with little or no change. Some remains are preserved when organisms become trapped in tar. Some remains are preserved when organisms become trapped in tar. Ancient organisms also have been preserved in amber. Amber is the hardened resin, or sap, of evergreen trees. Ancient organisms also have been preserved in amber. Amber is the hardened resin, or sap, of evergreen trees. Freezing is another way in which remains can be preserved. Freezing is another way in which remains can be preserved.

Preserved Remains

What do fossils tell about how organisms have changed over time? The fossil record provides evidence about the history of life on Earth. The fossil record also shows that different groups of organisms have changed over time. The fossil record provides evidence about the history of life on Earth. The fossil record also shows that different groups of organisms have changed over time. The fossil record reveals a surprising fact: fossils occur in a particular order. The fossil record reveals a surprising fact: fossils occur in a particular order. –Older rocks contain fossils of simpler organisms. Younger rocks contain fossils of more complex organisms. –In other words, the fossil record shows that life on Earth has evolved, or changed.

Fossil Record ewsdesk/extinction_04.jpg ges/trex2.gif

What do fossils tell about how organisms have changed over time? The fossil record provides evidence to support the theory of evolution. The fossil record provides evidence to support the theory of evolution. A scientific theory is a well-tested concept that explains a wide range of observations. A scientific theory is a well-tested concept that explains a wide range of observations. Evolution is the gradual change in living things over long periods of time. Evolution is the gradual change in living things over long periods of time. The fossil record shows that millions of types of organisms have evolved. The fossil record shows that millions of types of organisms have evolved. –But many others have become extinct. –A type of organism is extinct if it no longer exists and will never again live on Earth.

What do fossils tell about how organisms have changed over time? Paleontologists use fossils to build up a picture of Earth’s environments in the past. Paleontologists use fossils to build up a picture of Earth’s environments in the past. Fossils also provide evidence of Earth’s climate in the past. Fossils also provide evidence of Earth’s climate in the past. Scientists can use fossils to learn about changes in Earth’s surface. Scientists can use fossils to learn about changes in Earth’s surface.

INDEX FOSSIL EASILY IDENTIFIABLE WIDESPREAD OCCURRENCE SHORT-LIVED

Index Fossils To be an index fossil –an organism must have lived only during a short part of Earth’s history. To be an index fossil –an organism must have lived only during a short part of Earth’s history. Many fossils of the organism must be found in rock layers. Many fossils of the organism must be found in rock layers. The fossil must be found over a wide area of Earth; the organism must be unique. The fossil must be found over a wide area of Earth; the organism must be unique.

Index Fossils The shorter time period a species lived, the better an index it is. The shorter time period a species lived, the better an index it is. –A key example of an organism used as an index fossil are trilobites, a group of hard-shelled animals whose body had three sections, lived in shallow seas, and became extinct about 245 million years ago. –Therefore, if a trilobite is found in a particular rock layer, it can be compared with trilobites from other layers to estimate the age of the layer in which it was found.

Fossils Preserved fossils ambertarice Rock Fossils Trace fossils Casts and molds Petrified fossils Carbon films

In Summary Most fossils form when living things die and are quickly buried by sediment, which eventually hardens and preserves parts of the organisms. Most fossils form when living things die and are quickly buried by sediment, which eventually hardens and preserves parts of the organisms. The major kinds of fossils include petrified remains, molds, casts, carbon films, trace fossils, and preserved remains. The major kinds of fossils include petrified remains, molds, casts, carbon films, trace fossils, and preserved remains. The fossil record shows that many different organisms have lived on Earth at different times and that groups of organisms have changed over time. The fossil record shows that many different organisms have lived on Earth at different times and that groups of organisms have changed over time.