Glacier (?) National Park part of Pedagogy in Action:Partners::Examples
Judy McIlrath, University of South Florida
Spreadsheets Across the Curriculum/Geology of National Parks module. Students examine data about the disappearing glaciers in the park; after calculating percentage change in the number of glaciers from 1850 to 2000, they interpolate to estimate when Grinnell glacier will be gone.

What is the Discharge of the Congaree River at Congaree National Park? part of Pedagogy in Action:Partners::Examples
Denise Davis, University of South Florida-St. Petersburg
Spreadsheets Across the Curriculum module/Geology of National Parks course. Students use a rating curve to determine discharge at various stage heights.

Just How Faithful is Old Faithful? Finding Order in Random Behavior part of Pedagogy in Action:Partners::Examples
Module by: Tom Juster, University of South Florida Cover Page by: Len Vacher and Denise Davis, University of South Florida
Spreadsheets Across the Curriculum/Geology of National Parks Collection. Students create a histogram to examine the time between geyser eruptions of Old Faithful, Yellowstone National Park.

What Does the Mean Mean? Describing Eruptions at Riverside Geyser, Yellowstone National Park part of Pedagogy in Action:Partners::Examples
Module by: Tom Juster, University of South Florida Cover Page by: Len Vacher and Denise Davis, University of South Florida
Spreadsheets Across the Curriculum/Geology of National Parks module. Students study measures of central tendency in a bimodal dataset of eruption intervals.

Deciviews from Look Rock, Great Smoky Mountains National Park: How Hazy is it? part of Pedagogy in Action:Partners::Examples
, University of South Florida
Spreadsheets Across the Curriculum/Geology of National Parks module. Students calculate the haze index and standard visual range from concentrations of particulate matter.

Yellowstone! A National Park on a Hot Spot part of Pedagogy in Action:Partners::Examples
Module by: Judy McIlrath, University of South Florida Cover Page by: Len Vacher and Denise Davis, University of South Florida
Spreadsheets Across the Curriculum module/Geology of National Parks course. Students use foundational math to study the velocity of the North American Plate over the hot spot, the volume of eruptive materials from it, and the recurrence interval of the cataclysmic eruptions.

Comparing Stream Discharge in Two Watersheds in Glacier National Park part of Pedagogy in Action:Partners::Examples
Module by: Mark Rains, University of South Florida Cover Page by: Len Vacher and Denise Davis, University of South Florida
Spreadsheets Across the Curriculum module/Geology of National Parks course. Students study how discharge per unit area varies with elevation in the high country of Glacier National Park from USGS hydrograph data from Swiftcurrent Creek and its tributary Grinnell Creek..

Mapping Coastal Vulnerability to Sea-Level Rise at Point Reyes National Seashore part of Pedagogy in Action:Partners::Examples
, University of South Florida
Spreadsheets Across the Curriculum/Geology of National Parks module. Students work with a color-coded conditional-formatted spreadsheet map to work through a USGS report applying a coastal vulnerability index.

Salmon Use of Geomorphically Restored Streams at Point Reyes National Seashore part of Pedagogy in Action:Partners::Examples
Module by: Mark Rains, University of South Florida Cover Page by: Len Vacher and Denise Davis, University of South Florida
Spreadsheets Across the Curriculum module/Geology of National Parks course. Students work with salmon-trace streambed data to study whether removal of a spawning run barrier was effective

Mined-Over Matter: Remembering Copper Mining at Keweenaw National Historic Park, Upper Peninsula Michigan part of Pedagogy in Action:Partners::Examples
Module by: Judy McIlrath, University of South Florida Cover Page by: Judy McIlrath, Len Vacher, and Denise Davis, University of South Florida
Spreadsheets Across the Curriculum/Geology of National Parks module. Students calculate the amount of rock removed and the value of copper produced at the great Keweenaw District up to 1925.