U.S. DEPARTMENT OF THE INTERIOR
U.S. GEOLOGICAL SURVEY
Make Your Own Paper Model of a Volcano
Tau Rho Alpha and Leslie C. Gordon
Open-File Report 91-115B
Menlo Park, California
This report is preliminary and has not been reviewed for conformity with U. S. Geological survey editorial standards. Any use of trade, firm, or product names is for descriptive purposed only and does not imply endorsement by the U. S. government.
Although the program has been used by the U. S. Geological Survey, no warranty, expressed or implied, is made by the USGS as to the accuracy and functioning of the program and related program material, nor shall the fact of distribution constitute any such warranty, and no responsibility is assumed by the USGS in connection therewith.
A pdf version of this report is also
This report contains instructions and a pattern for making a three-dimensional paper model of a volcano. This model is intended to help students and others visualize a stratovolcano (inside and out) and to learn some of the terms used by geologists in describing it. By construction and examining the model, students will obtain a greater appreciation of the relationship between the internal structure of the volcano and its exterior shape and features. This exercise may give the student an insight as to how a stratovolcano is formed. Included in this report are the paper model, instructions for assembly, educators' guide, and a simple description of volcanoes.
The WWW version of this report includes a QuickTime animation of an erupting volcano. This animation was extracted from the HyperCard stack that was included with the diskette version of the original Open-file report, as described in the next paragraph.
Purchasers of the diskette version of this report, which includes all of the text and graphics, can use HyperCard 2.0 software (not supplied) to change the model (by adding geologic patterns, symbols, colors, etc.) or to transfer the model to other graphics software packages. Requirements for the diskette version are: Apple Computer Inc., HyperCard 2.0 software and Apple Macintosh Plus or later computer. The original publication date of this Open-file Report was February 4, 1991. OF 91-115-A, is a paper copy, with 3 pages. OF 91-115-B comes on a Macintosh 3.5 inch diskette. To order either of these versions of this report, contact: U. S. Geological Survey Books and Open-File Reports Sales, P. O. Box 25425, Denver, CO 80225, or call (303) 236-7476.
The pattern for making a paper model of volcano is available in these formats:
|File Format||Black and White||Color|
|GIF -- for printing from browser||volcano_bmod.gif||volcano_cmod.jpg|
|PDF -- for printing with the free Adobe Acrobat Reader software||volcano_bmod.pdf||volcano_cmod.pdf|
|DOC -- for printing with MS Word97||volcano_bmod.doc||volcano_cmod.doc|
QuickTime Volcano Eruption Movie
You will need to download a QuickTime player. Follow instructions on the Apple Site to obtain the QuickTime player for Apple, Windows 3.1 or Windows 95 computers.
For other platforms, players can be found on WWW sites such as WWW.SHAREWARE.COM.
The paper model in this report represents a stratovolcano, or composite volcano. It is the most common type of volcano on Earth. Scientists classify volcanoes into three main types: cinder cones, shield volcanoes, and stratovolcanoes (composite volcanoes).
Cinder cones are the smallest and have steep sides that are formed largely by the piling up of ash, cinders, and rocks. All of these materials are called pyroclastic ("fire-broken") and have been explosively erupted from the vent of the volcano. As the material falls back to the ground, it generally piles up to form a symmetrical, steep-sided cone around the vent. Sunset Crater in Arizona and Paricutin in Mexico are well-known examples of cinder cones.
Shield volcanoes are generally not explosive and are built by the accumulation of very fluid lava flows that spread out to produce a mountain with broad, gentle slopes. Shield volcanoes are the largest of all volcanoes, up to tens of kilometers across, and thousands of meters high. Kilauea and Mauna Loa Volcanoes in Hawaii are classic examples of active shield volcanoes.
A stratovolcano is built up of lava flows interlayered with pyroclastic material. Scientists believe that the layering represents a history of alternating explosive and quiet eruptions. Young stratovolcanoes are typically steep sided and symmetrically cone shaped. There are several active stratovolcanoes in North America. Since 1960, Mount Saint Helens in Washington has become the most familiar. Other will known stratovolcanoes in the United States include Mount Rainier, Mount Shasta, Mount Mazama (Crater Lake), and Redoubt Volcano in Alaska. Mount Fuji in Japan and Mount Vesuvius in Italy are other famous stratovolcanoes.
Questions for Further Study
|Discuss the meanings and usage of the following words with your class.|
|stratovolcano||cinder cone||composite volcano||lava|
|shield volcano||vent||volcanic hazard||eruption|
Crandell, D. R., and Nichols, D. R., 1987, Volcanic Hazards at Mount Shasta, California, U. S. Geological Survey General Interest Publication, 21p.
Heliker, C., 1990, volcanic and seismic Hazards on the Island of Hawaii: U. S. Geological Survey General Interest Publication, 48p.
Simkin, T., tilling, R. I., Taggart, J. N., Jones, W. J., and Spall, H., compilers, 1989, this Dynamic Planet: World Map of Volcanoes, Ear4thquakes, and Plate Tectonics: U. S. Geological Survey, Reston, VA, in cooperation with the Smithsonian Institution, Washington, D. C.
Tilling, R. I., 1982, Volcanoes: U. S. Geological Survey General Interest Publication, 45p.
Tilling, R. I., Heliker, C., and Wright, T. L., 1987, Eruptions of Hawaiian volcanoes: Past, Present and Future: U. S. Geological Survey General Interest Publication, 54p.
Tilling, R. I., Topinka, L., and Swanson, D. A., 1984, revised 1990, Eruptions of Mount St. Helens: Past, Present, and Future: U. S. Geological Survey General Interest Publication, 57p.
This document was converted from the HyperCard stack to HTML and QuickTime by John C. Lahr. (Email: email@example.com)