In this classroom activity, young students compare their feet to the foot of a large Apatosaur. The activity opens with background information for teachers about the enormous size range of dinosaurs. After using personal references to describe the size of dinosaurs, students examine the outline of an Apatosaur footprint. Students then estimate how many of their footprints would fit inside the Apatosaur footprint and conduct an experiment to test their estimate.

This activity is an observational activity where students observe differnt fossils and predict what they are seeing and how old it might be.

This course examines the dynamic interrelations among physical and behavioral traits of humans, environment, and culture to provide an integrated framework for studying human biological evolution and modern diversity. Topics include issues in morphological evolution and adaptation; fossil and cultural evidence for human evolution from earliest times through the Pleistocene; evolution of tool use and social behavior; modern human variation and concepts of race. The class also studies stone artifacts and fossil specimens.

This site assembles the information from the April 1997 American Museum of Natural History symposium on the role humans have played, and continue to play, in the extinction of species. It presents an overview of extinction, the various hypotheses that explain this irreplaceable loss, details about what happened 14,000 years ago and the ongoing role humans play in the extinction process, a bestiary with notes and illustrations about some of the mammals that have gone extinct from the Pleistocene era through the 20th century, and what can be done to prevent another extinction event.

This activity is a geology lab where students learn about fossils found in sedimentary rocks and show their understanding by writing a literary nonfiction paper from the perspective of one of those fossils.

By presenting the students with fossils and other earth materials and giving clues as to their origin, they will be able to identify the fossils and materials and be able to form a hypothesis as to how they were formed and what it was before preservation.

Geology is the core discipline of the earth sciences and encompasses many different phenomena, including plate tectonics and mountain building, volcanoes and earthquakes, and the long-term evolution of Earth’s atmosphere, surface and life. Because of the ever-increasing demand for resources, the growing exposure to natural hazards, and the changing climate, geology is of considerable societal relevance. This course introduces students to the basics of geology. Through a combination of lectures, labs, and field observations, we will address topics ranging from mineral and rock identification to the origin of the continents, from geologic mapping to plate tectonics, and from erosion by rivers and glaciers to the history of life.

Geology is the core discipline of the earth sciences and encompasses many different phenomena, including plate tectonics and mountain building, volcanoes and earthquakes, and the long-term evolution of Earth’s atmosphere, surface and life. Because of the ever-increasing demand for resources, the growing exposure to natural hazards, and the changing climate, geology is of considerable societal relevance. This course introduces students to the basics of geology. Through a combination of lectures, labs, and field observations, we will address topics ranging from mineral and rock identification to the origin of the continents, from geologic mapping to plate tectonics, and from erosion by rivers and glaciers to the history of life.

In this activity, students organize a set of fossils chronologically and learn to correlate, based on fossil evidence, the stratigraphy of one location with that of an adjacent location. Earth Science Reference Tables are used to identify the epoch of occurrence and the age of each of the fossil specimens. Students will become familiar with the concept of index fossils and understand what makes a good index fossil.

1) What do you think it means for a fossil resource to be "abused"?

2) What's the issue with fossil hunting on federal land (such as National Parks)? Explain what your interpretation of the conflict is.

3) Do you think commercial dealers and scientists can work together? How? Is this a good idea?

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This lesson uses the fundamentals of protein synthesis as a context for investigating the closest living relative to Tyrannosaurus rex and evaluating whether or not paleontologist and dinosaur expert, Jack Horner, will be able to "create" live dinosaurs in the lab. The first objective is for students to be able to access and properly utilize the NIH's protein sequence database to perform a BLAST, using biochemical evidence to determine T rex's closest living relative. The second objective is for students to be able to explain and evaluate Jack Horner's plans for creating live dinosaurs in the lab. The main prerequisite for the lesson is a basic understanding of protein synthesis, or the flow of information in the cell from DNA to RNA during transcription and then from RNA to protein during translation

This article highlights children's literature about fossils, dinosaurs, archaeology, and paleontology for use in the elementary classroom.

This activity is a combination outdoor/indoor lab where students will collect natural materials from the environment and use them to create both a mold and cast model of a fossil. Students will learn how a fossil is formed and why scientists use models to help them understand how things work and develop.

This lesson is a classroom activity where students learn about paleontologist Mary Anning, briefly learn about sedimentary rock, and complete observation drawings of Platteville Limestone fossils.

When scientists discover a new fossil skull, they compare it to skulls that have already been identified as particular early human species. In this activity, you get the chance to be the scientist!

The Champlain Lowlands tour is part of the New York Landscape Regions Collection of Google Earth tours, created by a group of New York State science educators. This tour includes views of the gorge of the Ausable River, cut through Late Cambrian Potsdam Sandstone, and the geology of the Champlain Thrust Fault, a low angle thrust fault formed as the proto-Atlantic Ocean closed during the Taconic Oregeny. When it was still connected to the ocean, Lake Champlain was home to whales, whose fossils are now entombed in the lake sediments. The tour also includes classroom activities for students.

This Ology website for kids focuses on Paleontology. It includes activities, things to make, quizzes, interviews with working scientists, and more to help kids learn about Paleontology.

For this homework assignment, students have to draw two scaled timelines. The first is a personal timeline. They need to come up with the events themselves, an easy task that will build confidence for student who are intimidated by science and math. Following guidelines, they decide on a scale, and draw a linear timeline on which they plot their chosen events. Most students will primarily include recent events. They are asked to identify and explain any patterns in their timeline. Students should note the clustering at the present, and describe the emphasis on the present as resulting from memory, relevance to future hopes and worries, etc.

The second timeline is more traditional. The students are given 16 Earth history events with dates and asked to draw another timeline, using the procedure from the personal timeline, but the line is already drawn for them. They will probably recognize most of the events on the list, and will be keeping them in order and spacing them out on the timeline. They are once again asked to identify and explain patterns and should recognize the emphasis on the present. This time, availability of fossils/rocks and relevance to current conditions and problems are good answers.

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Survey of the important aspects of modern sediments and ancient sedimentary rocks. Emphasis is on fundamental materials, features, and processes. Textures of siliciclastic sediments and sedimentary rocks: particle size, particle shape, and particle packing. Mechanics of sediment transport. Survey of siliciclastic sedimentary rocks: sandstones, conglomerates, and shales. Carbonate sediments and sedimentary rocks; cherts; evaporites. Siliciclastic and carbonate diagenesis. Paleontology, with special reference to fossils in sedimentary rocks. Modern and ancient depositional environments. Stratigraphy. Sedimentary basins. Fossil fuels: coal, petroleum.