Sedimentary Petrology Field Trip to Gravel Quarry near Rotterdam Junction, NY
Summary
Sedimentary Petrology: one field trip involves visiting an exceptional glacial outwash gravel quarry, where students measure, identify and count clast types, measure cross-bedding directions, and examine the early stages of lithification of gravel to conglomerate. The gravel deposits are also representative of the local surficial aquifer material that lies nearby in the subsurface
Context
Audience
This is a field trip activity (2-3 hours) for an upper level undergraduate class in sedimentary petrology
Skills and concepts that students must have mastered
Students must have completed a course in Physical Geology with lab. They must be able to identify various types of rocks (and minerals in them) in hand samples
How the activity is situated in the course
This activity is conducted at one field trip stop on a required weekend field trip in sedimentary petrology to eastern NY and New England
Goals
Content/concepts goals for this activity
- Students should be able to interpret the relationships of sedimentary deposits from glacial and fluvial systems
- Students should be able to analyze the concept of provenance of sedimentary clasts
- Students should be able to analyze the relationships of clast size and shape to sediment transport
- Students should be able to analyze the concept of cementation in sedimentary deposits
Higher order thinking skills goals for this activity
- Students should be able to interpret changes in deposition through time
- Students should be able to interpret regional change in paleogeography with time
Other skills goals for this activity
- Students should be able to improve rock and mineral identification skills
- Students should be able to improve on field data collection skills
- Students should be able to work effectively in small groups
Description of the activity/assignment
This is a Stratigraphy Sedimentary Petrology field trip stop at an exceptional glacial outwash gravel quarry, where students measure, identify and count clast types, measure cross-bedding directions, and examine the early stages of lithification of gravel to conglomerate. The gravel deposits are also representative of the local surficial aquifer material that lies nearby in the subsurface.
Determining whether students have met the goals
Students will be evaluated using the categories of "exceeds," meets," or "does not meet" all of the goals stated above
More information about assessment tools and techniques.Teaching materials and tips
- Sedimentary Petrology Field Trip to Gravel Quarry near Rotterdam Junction, NY (Microsoft Word 21kB May24 10)
- INSTRUCTOR NOTES (Microsoft Word 24kB May24 10)
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