# QR Teaching Activities

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# Quantitative Skills

- Algebra 4 matches
- Arithmetic/Computation 13 matches
- Differential Equations and Integrals 7 matches
- Estimation 9 matches
- Fourier Series, Spectral Analysis 1 match
- Fractions and Ratios 2 matches
- Gathering Data 1 match
- Geometry and Trigonometry 7 matches
- Graphs 5 matches
- Logarithms/Exponential Functions 6 matches
- Models and Modeling 6 matches
- Probability and Statistics 13 matches
- Problem Solving 13 matches
- Scientific Notation 1 match
- Units and Unit Conversions 10 matches

Results 1 - 10 of **31 matches**

Back-of-the-Envelope Calculations: Weight of Gold part of Quantitative Skills:Activity Collection

Barb Tewksbury, Hamilton College

Question Let's suppose that you have a shoe box full of water (the box is waterproof, of course). The shoe box weighs about 9 kg (19.8 pounds). Suppose you emptied the box and filled it completely with rock ...

Porosity and Permeability of Magmas part of Pedagogy in Action:Partners:Spreadsheets Across the Curriculum:Physical Volcanology:Examples

chuck connor

SSAC Physical Volcanology module. Students build a spreadsheet for an iterative calculation to find volume of bubbles and hence porosity, permeability and gas escape as a function of depth.

What is the Volume of the 1992 Eruption of Cerro Negro Volcano, Nicaragua? part of Pedagogy in Action:Partners:Spreadsheets Across the Curriculum:Physical Volcanology:Examples

chuck connor

SSAC Physical Volcanology module. Students build a spreadsheet to calculate the volume a tephra deposit using an exponential-thinning model.

What is the Volume of a Debris Flow? part of Pedagogy in Action:Partners:Spreadsheets Across the Curriculum:Physical Volcanology:Examples

chuck connor

SSAC Physical Volcanology module. Students build a spreadsheet to estimate the volume of volcanic deposits using map, thickness and high-water mark data from the 2005 Panabaj debris flow (Guatemala).

How Does Surface Deformation at an Active Volcano Relate to Pressure and Volume Change in the Magma Chamber? part of Pedagogy in Action:Partners:Spreadsheets Across the Curriculum:Physical Volcanology:Examples

Module by Peter LaFemina, Penn State, State College, PA. This cover page by Ali Furmall, University of South Florida, now at University of Oregon.

SSAC Physical Volcanology module. Students build a spreadsheet to examine and apply the Mogi model for horizontal and vertical surface displacement vs. depth and pressure conditions in the magma chamber.

How Do We Estimate Magma Viscosity? part of Pedagogy in Action:Partners:Spreadsheets Across the Curriculum:Physical Volcanology:Examples

chuck connor

SSAC Physical Volcanology module. Students build a spreadsheet to examine how magma viscosity varies with temperature, fraction of crystals, and water content using the non-Arrhenian VFT model.

Bubbles in Magmas part of Pedagogy in Action:Partners:Spreadsheets Across the Curriculum:Physical Volcanology:Examples

Module by Chuck Connor, University of South Florida, Tampa. This cover page by Ali Furmall, USF, now at U. Oregon.

SSAC Physical Volcanology module. Students build a spreadsheet and apply the ideal gas law to model the velocity of a bubble rising in a viscous magma.

The Floating Lithosphere - Isostasy part of Quantitative Skills:Activity Collection

Len Vacher, Dept of Geology, University of South Florida

Students are asked to numerically and then analytically determine the relations governing the depth of compensation.

Sonar Demonstration -- Human Sound Wave part of Cutting Edge:Courses:Oceanography:Activities

Kent Syverson, University of Wisconsin-Eau Claire

Sonar technology allowed scientists to produce high-resolution maps of the sea floor for the first time. This sonar demonstration uses a Human Sound Wave to image the "sea floor" in a lecture hall. In ...

The Floating Lithosphere - Isostasy part of Quantitative Skills:Activity Collection

Len Vacher, Dept of Geology, University of South Florida

Students are asked to numerically and then analytically determine the relations governing the depth of compensation.