1
This activity introduces students to the concept of sorting materials in different mediums and the sedimentary feature called graded bedding. Students will discover that water is a good medium to separate and sort particles, and that particles behave differently in water than in air.
Grade Level   7 8 9 10 11 12
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2
Because the formation of soil involves the interaction of numerous physical, chemical, and biological processes, the study of soil provides an unmatched opportunity to illustrate connections between science and a systems approach to understanding earth processes. Soil, as the basis for agriculture,...
Grade Level   7 8 9 10 11 12
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3
Paper models of crystals and cleavage. PDF, printable.
Grade Level   9 10 11 12
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4
Next time you teach plate tectonics, consider a Draw With Me presentation that will engage your students and help them understand the spatial and movement aspects of plate boundary environment. This website provides illustrations that students can color to help them better learn about plate...
Grade Level   6 7 8 9 10 11 12
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5
"""""""""Although Alfred Wegener was not the first to suggest that continents have moved about The Earth, his presentation of carefully compiled evidence for continental drift inspired decades of scientific debate. Wegener's evidence, in concert with compelling evidence provided by post World War II...
Grade Level   6 7 8 9 10
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6
Students will use a chemical reaction to test for the presence of carbonate in calcite and limestone. By dropping a small amount of an acid on these specimens, they will observe bubbles of carbon dioxide forming from the reaction of the acid with carbonate minerals.
Grade Level   9 10 11 12
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7
Potholes like the ones featured in this activity may have been formed by the grinding action of pebbles being swirled round by the fast-moving water. We can re-create these conditions by swirling pebbles in a bucket of water, using a spade.
Grade Level   9 10 11 12
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8
Published in 1994
Students often ask how scientists know that the continents have moved. This activity about the apparent wandering of the North Pole provides good evidence that the continents do indeed move.
Grade Level   9 10 11 12
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9
Using a pupil model to demonstrate the slab pul is the main plate-driving force. Considering the different processes likely to be driving plate movement by use os a student model.
Grade Level   9 10 11 12
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10
Hand modelling of compression, tension, and shear in the Earth. A class activity to help pupils to visualize types of stress in the Earth through modelling with their hands.
Grade Level   9 10 11 12
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11
This activity can be used as one means of explaining isostasy, in the context of the Earth's structure and its surface relief. Students will model the principle of isostasy with wooden blocks.
Grade Level   11 12
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12
In this lesson, students will create three-dimensional (3-D) blocks out of paper to learn about the types of faulting that occur at the Earth’s surface and its interior, and explain how earthquakes are generated by fault movement. Step-by-step directions will provide students with the necessary...
Grade Level   K 1 2 3 4 5 6 7 8 9 10 11 12
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13
Published in 1990
This report contains instructions and patterns for preparing seven, 3-D paper models that schematically illustrate common earth faults and associated landforms. The faults described are: normal, reverse, right- and left-lateral strike-slip, and oblique-slip. There are also models and discussions of...
Grade Level   6 7 8 9 10 11 12
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14
This PDF has three useful worksheets for students on characteristics of Igneous, Sedimentary, and Metamorphic rocks.
Grade Level   5 6 7 8 9 10 11 12
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15
By GeoBlox
This 3-D earthquake model demonstrates parts of an earthquake: the focus, the epicenter, and P waves.
Grade Level   6 7 8 9 10 11 12
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16
Published in 1993
This report contains instructions and two patterns for making a terrestrial globe and a tectonic globe. The pattern or map projection is designed to be glued onto a used tennis ball. The terrestrial globe is intended to help visualize the location of the continents and oceans. The purpose of the...
Grade Level   3 4 5 6 7 8 9 10 11 12
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17
Published in 1997
This report illustrates how dinosaurs may have become extinct as a result of an asteroid impact. Students will better understand the mass extinctions that have been part of the Earth's history. Included are templates for making two paper models, instructions for their assembly, and a discussion of a...
Grade Level   6 7 8 9 10 11 12
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18
Published in 1991
This report contains instructions and patterns for preparing a set of four, 3-D paper models that schematically illustrate the development of island coral. The first model is of a shield volcano that extends above sea level, making a volcanic island. The second is of the original shield volcano and...
Grade Level   9 10 11 12
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19
Published in 1998
This report illustrates why sand dunes can develop different forms. Students will better understand the evolution of sand dunes. Included are templates for making a paper model, instructions for their assembly, and a discussion of development of different forms of sand dunes.
Grade Level   6 7 8 9 10 11 12
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20
Published in 1997
This report illustrates why caves develop in limestone. Students will better understand the evolution of Karst topography. Included are templates for making a paper model, instructions for its assembly, and a discussion of development of Karst topography.
Grade Level   6 7 8 9 10 11 12
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