Seventh grade Lesson Relative Age of Rocks

Britannica does not currently have an article on this topic. The topographic expressions of eroded anticlines and synclines. Three basic fault types: The forms of three types of folds. Two transform faults offsetting a mid-oceanic ridge. Volcanic activity and the Earth’s tectonic plates Stratovolcanoes tend to form at subduction zones, or convergent plate margins, where an oceanic plate slides beneath a continental plate and contributes to the rise of magma to the surface. At rift zones, or divergent margins, shield volcanoes tend to form as two oceanic plates pull slowly apart and magma effuses upward through the gap. Volcanoes are not generally found at strike-slip zones, where two plates slide laterally past each other. Crustal abundances of elements of atomic numbers 1 to

Phoenicians Worksheets

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Geologic History Reference Tables – The Mesozoic began million years ago and ended 65 million years ago – this is a time period of million years. If cm = 10 million years, then.

Interpret successive layers of sedimentary rocks and their fossils to infer relative ages of rock sequences, past geologic events, changes in environmental conditions, and the appearance and extinction of life forms. Use relative dating techniques to explain how the structures of the Earth and life on Earth have changed over short and long periods of time.

Explain how rocks and fossils are dated. Understand the geologic time scale and Earth’s history. Must be present in class to earn points for notes. Day 1- Fossils Section Make a poster showing the process by which fossils form VS-5 pts. Pretend you are an animal.

Evolution: Library: Radiometric Dating

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The Age of Dinosaurs was so many millions of years ago that it is very difficult to date exactly. Scientists use two kinds of dating techniques to work out the age of rocks and fossils. The first method is called relative dating. This considers the positions of the different rocks in sequence (in.

Dating techniques Photo by: Bastos Dating techniques are procedures used by scientists to determine the age of an object or a series of events. The two main types of dating methods are relative and absolute. Relative dating methods are used to determine only if one sample is older or younger than another. Absolute dating methods are used to determine an actual date in years for the age of an object. Relative dating Before the advent of absolute dating methods in the twentieth century, nearly all dating was relative.

The main relative dating method is stratigraphy pronounced stra-TI-gra-fee , which is the study of layers of rocks or the objects embedded within those layers. This method is based on the assumption which nearly always holds true that deeper layers of rock were deposited earlier in Earth’s history, and thus are older than more shallow layers. The successive layers of rock represent successive intervals of time.

Since certain species of animals existed on Earth at specific times in history, the fossils or remains of such animals embedded within those successive layers of rock also help scientists determine the age of the layers. Similarly, pollen grains released by seed-bearing plants became fossilized in rock layers. If a certain kind of pollen is found in an archaeological site, scientists can check when the plant that produced that pollen lived to determine the relative age of the site.

Absolute dating Absolute dating methods are carried out in a laboratory. Absolute dates must agree with dates from other relative methods in order to be valid.

Seventh grade Lesson Relative Age of Rocks

In the very beginning of earth’s history, this planet was a giant, red hot, roiling, boiling sea of molten rock – a magma ocean. The heat had been generated by the repeated high speed collisions of much smaller bodies of space rocks that continually clumped together as they collided to form this planet. As the collisions tapered off the earth began to cool, forming a thin crust on its surface.

As the cooling continued, water vapor began to escape and condense in the earth’s early atmosphere. Clouds formed and storms raged, raining more and more water down on the primitive earth, cooling the surface further until it was flooded with water, forming the seas.

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Geologists have calculated the age of Earth at 4. But for humans whose life span rarely reaches more than years, how can we be so sure of that ancient date? It turns out the answers are in Earth’s rocks. Even the Greeks and Romans realized that layers of sediment in rock signified old age. But it wasn’t until the late s — when Scottish geologist James Hutton, who observed sediments building up on the landscape, set out to show that rocks were time clocks — that serious scientific interest in geological age began.

Before then, the Bible had provided the only estimate for the age of the world:

History of life on Earth

Giant impact hypothesis The Earth’s relatively large natural satellite , the Moon , is unique. The Moon has a bulk composition closely resembling the Earth’s mantle and crust together, without the Earth’s core. This has led to the giant impact hypothesis: Theia finally collided with Earth about 4. This material would eventually form the Moon. However, the metallic cores of the impactor would have sunk through the Earth’s mantle to fuse with the Earth’s core, depleting the Moon of metallic material.

Earth Science Chapter 10 Layered Assignments. A Trip Through Geologic Time. Alan Dewey Wabasso High School. OBJECTIVES 1. Interpret successive layers of sedimentary rocks and their fossils to infer relative ages of rock sequences, past geologic events, changes in environmental conditions, and the appearance and extinction of life forms.

Hide This activity has benefited from input from a review and suggestion process as a part of an activity development workshop. This activity has benefited from input from faculty educators beyond the author through a review and suggestion process as a part of an activity development workshop. Workshop participants were provided with a set of criteria against which they evaluated each others’ activities. For information about the criteria used for this review, see http: This page first made public: Mar 14, Summary In this classroom activity, students first use an interview with an older adult to construct a timescale.

Students use criteria of their choosing to divide the timescale into periods, then compare and contrast timescales among the class. Students are next given important events in the history of the earth and are invited to first develop a scaled representation of the earth’s history based on their prior knowledge. Students then use classroom and Internet resources to place the same events in the proper order and at the correct locations along the timescale.

Finally, students investigate the geologic timescale and place eons and eras of geologic time on the same scale as earth events. Comparisons are drawn between the human life timescale and geologic time. For assessment, the instructor grades written student responses to questions in the student course pack. The student course pack activity and instructor notes are provided.

Learn more about the course for which this activity was developed.

Earth Worksheets

Volcanic time markers – a layer of volcanic dust covering layers. When a violent eruption of a volcano occurs it may send dust high into the atmosphere where it can spread over the entire planet. It settles out of the air and forms a layer over wide regions at the same time. Asteroid impacts can have the same effect.

Methods of establishing the age of materials include the technique known as radioactive dating. Recall that the atomic number of an element is the number of protons in the nucleus. All atoms of an element have the same atomic number, but their number of neutrons can vary.

Scientists are rarely able to perform an experiment and obtain meaningful results within a time frame of one or two class periods. The following investigations require an extended period of time. In performing these projects, students should have the opportunity to observe change, gather data, record information, and make conclusions about the world around them.

Some students may use this list of viable investigations to generate their own project ideas, but the teacher should approve all projects before they are conducted. Although library research is an important aspect of nearly any scientific inquiry, students are strongly encouraged to make the gathering and analysis their own observations and data the primary emphasis of their long-term projects.

Establish communication that will enable you to measure the size of the Earth through a computer link with a number of other schools. Measure the quantity of air-borne particulate pollution at a number of locations. Correlation of your data with wind directions and time of year may also be appropriate. This is a good opportunity to show your skills in drawing isolines.

Layered Chapter 10 Geologic

Draw Figure 1 on the classroom board, or show students a suitable diagram or projected image. The inner core, mantle and crust are solid, and the outer core is molten, or liquid. The crust is the thinnest layer of the Earth and is the layer on which we live. The inner core, outer core and mantle experience extremely high pressures and temperatures.

Formation of the Earth In human terms, the age of the Earth is immense. The Earth and solar system were modern dating techniques that it is 4, million years old. To put this into perspective, Geologists date events in Earth’s history by measuring tiny amounts of radioactive elements (e.g. uranium) in certain types of rocks.

Early history[ edit ] In Ancient Greece , Aristotle BCE observed that fossils of seashells in rocks resembled those found on beaches — he inferred that the fossils in rocks were formed by living animals, and he reasoned that the positions of land and sea had changed over long periods of time. Leonardo da Vinci — concurred with Aristotle’s interpretation that fossils represented the remains of ancient life. Steno argued that rock layers or strata were laid down in succession, and that each represents a “slice” of time.

He also formulated the law of superposition, which states that any given stratum is probably older than those above it and younger than those below it. While Steno’s principles were simple, applying them proved challenging. Steno’s ideas also lead to other important concepts geologists use today, such as relative dating. Over the course of the 18th century geologists realized that: Sequences of strata often become eroded, distorted, tilted, or even inverted after deposition Strata laid down at the same time in different areas could have entirely different appearances The strata of any given area represented only part of Earth’s long history The Neptunist theories popular at this time expounded by Abraham Werner — in the late 18th century proposed that all rocks had precipitated out of a single enormous flood.

John McPhee asserts that “as things appear from the perspective of the 20th century, James Hutton in those readings became the founder of modern geology”. This theory, known as ” Plutonism “, stood in contrast to the “Neptunist” flood-oriented theory. Formulation of geologic time scale[ edit ] The first serious attempts to formulate a geologic time scale that could be applied anywhere on Earth were made in the late 18th century. The most influential of those early attempts championed by Werner , among others divided the rocks of Earth’s crust into four types: Primary, Secondary, Tertiary, and Quaternary.

Each type of rock, according to the theory, formed during a specific period in Earth history.

Relative and Absolute Dating