101
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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102
Published in 2016
Compaction of soil can contribute to size and numbers of pores. Soil can become compacted many ways, and this can have long-term effects. For example, when American settlers traveled the Oregon Trail in their wagons in the 1800s, soil became so compacted that we still can see wheel ruts today. Try...
Grade Level   5 6 7 8 9 10
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103
Demonstrating how seismic shaking depends on local geology.
Grade Level   7 8 9 10 11 12
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104
Students use paper plates with various phases to create a three dimensional model of the lunar phases relative to the Earth and Sun, as both an assessment of their understanding and to continue to build a conceptual model through kinesthetic activities.
Grade Level   5 6 7 8 9 10 11 12
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105
The students create kinesthetic models of the Sun and Moon in the sky to better understand the relationshop between lunar phases and the time of day.
Grade Level   6 7 8 9 10 11 12
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106
Published in 2014
These drafts were written to help delve more deeply into the explanations and descriptions for why we have lunar phases; while the style is similar to other probes, these have not been through the extensive testing done by NSTA's assessment probes.
Grade Level   4 5 6 7 8 9 10 11 12
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107
In this kinesthetic acticity, students model how the Moon's gravitational pull causes the level of the ocean to rise and fall twice a day along most coastlines.
Grade Level   6 7 8 9 10 11 12
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108
Coal produces more than half of the electricity used in the United States, and is our most abundant domestic nonrenewable energy source. The students will comupte the cost of electricity used to light their classroom and their school for one hour through one year, the number of kilowatt ours of...
Grade Level   5 6 7 8 9 10 11 12
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109
By GeoBlox
Groins are artificial structures built along coastlines to help widen developed beaches, and so help the local tourist industry. This groin model can be attached to other models to make one long, continuous beachfront.
Grade Level   7 8 9 10 11 12
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110
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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111
By GeoBlox
Jetties are man-made structures that are built along coastlines to control the deposition of sediments at the mouths of stream channels. This model demonstrates how jetties work.
Grade Level   8 9 10 11 12
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112
By GeoBlox
Layers of the ocean crust are demonstrated through this paper model.
Grade Level   6 7 8 9 10 11 12
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113
By GeoBlox
An oasis forms when precipitation falling in the recharge zone seeps into the ground where porous and permeable rocks are found at the surface. This groundwater may travel many miles through the aquifer and resurface where the porous layer is exposed. When this occurs in a desert region an oasis may...
Grade Level   6 7 8 9 10 11 12
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114
By GeoBlox
This is a color version of a composite cone (stratovolcano) paper model.
Grade Level   5 6 7 8 9 10 11 12
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115
By GeoBlox
This is a black and white version of a composite cone (stratovolcano) paper model.
Grade Level   5 6 7 8 9 10 11 12
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116
By GeoBlox
Jones Spring is located in the bed of the intermittent stream Walnut Creek. Walnut Creek is also a disappearing stream. Water flows down along the Hensell Sand Member in the bed of Walnut Creek until it reaches the contact with the Cow Creek Limestone. This limestone is a coquina that formed from...
Grade Level   8 9 10 11 12
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117
This activity can be used in any science or geography lesson about the processes and products of the sedimentary rock cycle.
Grade Level   7 8 9 10 11 12
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118
Using a stress ball, needle and thread, and a small magnet, students can craft their own magnetic Earth.
Grade Level   7 8 9 10 11 12
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119
Earthquakes create seismic waves that travel through the Earth. By analyzing these seismic waves, seismologists can explore the Earth's deep interior.
Grade Level   K 1 2 3 4 5 6 7 8 9 10 11 12
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120
An earthquake causes different types of energy to radiate from the epicenter. The P and S waves are the first two to arrive at any specific point. P and S waves have different motions and shake the earth differently as they travel through it. In this activity, students demonstrate the motions of S...
Grade Level   K 1 2 3 4 5 6 7 8 9 10 11 12
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