This activity will help students to explore characteristics of microbes that live in the deep sea. This activity can be conducted as a jigsaw or research project, and can be used with face-to-face, remote, and hybrid students.

Provenance: Beverly Owens, Cleveland Early College High School
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This activity is a Google Slide playlist that will introduce students to microbes that can be found in deep sea sediments, and what roles they play in their environment. This playlist is suitable for use in remote, hybrid, or in-person instruction and can easily be added to a Learning Management System.

Provenance: Molly Ludwick, Kings Mountain Middle School
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Appreciating the depth of time is a bit like trying to understand the national debt -- it is easy to rattle off the number, but more difficult to appreciate what it means. Several popular writers have tried to convey the depth of time by incoporating one major (and important!) signpost in their scales: the first historical records of humans on the planet. Mark Twain famously referred to human history as the "skin of paint" at the summit of the Eiffel Tower, and John McPhee the "stroke of a medium-grained nail file" on the middle nail of an outstretched arm.

Eiffel Tower


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Vitruvian man


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I would like for you to evaluate these two metaphors for accuracy. How close were Twain and McPhee to appropriately contexualizing human existence in geological time? Use the pdf's of Twain's and McPhee's prose and what you know from class lectures to accomplish the following goals.

(1) Evaluate whether McPhee's and Twain's metaphors are appropriately scaled -- i.e., do their metaphors correctly depict the age of the earth relative to human history? How about if we incorporate the fossil record of humans?

(2) Create your own appropriately scaled metaphor. Add in at least three other "signposts", either biological or geological, into your metaphor and explain why you chose them.

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This activity is designed to introduce students to the way in which thermohaline circulation and the biological pump influence the distribution of nutrients, oxygen, carbon, and radiocarbon in the Atlantic vs. Pacific Oceans.

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This page explains the position in defense of the Black Hills. The purpose is to ensure that the Fort Laramie Treaties are re-upheld.

Students match microstructures to the deformation mechanisms by which they form; compare pairs of photomicrographs chosen to highlight key differences between some common microstructures; and complete a self-quiz in which they identify microstructures and infer deformation mechanisms from photomicrographs.

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This assignment addresses cultural sustainability by asking students to go beyond distinguishing between five subsistence strategies to examining the impact of globalization on diet and culture.

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Students are given 4 hypothetical stratigraphic columns (each roughly 30 m thick) of deltaic deposits, 3 base maps with section locations, and a map scale. Students subdivide the stratigraphic units into subfacies and interpret subenvironments (delta plain, delta front, prodelta, marine) and describe/list features used to make these interpretations. Using depositional interpretations, 3 bentonite marker beds, and paleocurrent information, students draw 3 successive paleogeographic maps of the region showing delta migration through time.

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A demonstration (with full class participation) to illustrate radioactive decay by flipping coins. Shows students visually the concepts of exponential decay, half-life and randomness. Works best in large classes -- the more people, the better.

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One of the great challenges in teaching undergraduates is finding ways to get them to apply knowledge or skills learned in one class to problems encountered in subsequent classes. Case in point: the use of algebra, trig, and even rudimentary calculus in geology classes! This activity presents practical ways we can use to build student confidence in their ability to peer into the meaning of the equations they encounter in sedimentary geology. These techniques include: (1) Surgical Strike Reviews -- 5 to 10-minute review of relevant math principles at the beginning of the appropriate lecture, (2) Unit Analyses -- assigning fundamental units of Mass, Length, and Time to test whether an equation has been derived correctly or to explore the meaning of derivative units of measure that may be unfamiliar to students, and (3) Perturbation Interrogation -- asking students to identify whether the quantity of interest described by an equation will increase or decrease when individual components of the equation increase or decrease.

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This 3-hour hands-on guided-discovery lab activity teaches students the concepts of density, buoyancy, thermal expansion and convection.

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In this lab activity, students determine density differences of water samples with varying temperature and salinity levels. Students synthesize information to predict the effects of oil in given water samples.

This hands-on lab activity is designed to teach students about how density differences, due to salinity, drive the flow of currents in the ocean. It also helps develop skills in performing and designing simple laboratory measurements; data entry, calculations and graph plotting in a spreadsheet; and comparing experimental data with a theoretical equation.
Key words: ocean circulation; density driven flows; salinity; ocean density; thermohaline circulation.

Density, Isostasy, and Topography Anne Egger, Stanford University The original activity Density, Isostasy, and Topography already exists within the SERC website. This page describes how this activity can be used ...

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HideA critical component of this activity involves sharing team data with the entire class, done the old-fashioned way on the chalkboard. Details This activity begins with an exploration of a topographic map of the earth, ending with the question: Why is the distribution of topography on the earth bimodal? The students then collect two forms of data. They measure the density of the most common rocks that make up oceanic crust (basalt), continental crust (granite), and the mantle (peridotite). They also measure the density of several different kinds of wood, and how high each kind floats in a tub of water. In each case, they work in teams of two or three and then the entire class shares their data. Based on the data from the wood, they derive an equation that relates the density of the wood to the height at which the block floats in the water - the isostasy equation. They then substitute density values for real rocks into their equation to derive thicknesses for average continental and oceanic crust, and apply their knowledge in order to draw a cross-section of the crust across South America. This activity gives students a real, hands-on and mathematical understanding of the principle of isostasy.

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A lab where the students study the density of pennies. They will discover the limitations of measurements and the value of multiple trials.

River and wind processes can be readily studied in the field, and we have devised a series of lab exercises in western Nevada that take advantage of our rivers and deserts. But for density-contrast flows, there was no easy way to get the students beyond pictures and formulae. With the assistance of Tripp Plastics, we designed acrylic tanks that fit on a lab bench. They have a ramp with screw-adjustable slope up to 20Â. Students mix a solution of Epsom salt (MgSO4) to several experimental densities. They add a dye to make the dense fluid visible. The dyed fluid is released at the top of the slope. The grid allows the flow to be accurately timed and described. The students determine how density changes and how slope affect the flow velocity and structure.

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This activity modifies a typical density laboratory exercise to fit within a lecture session. Students are asked to compare the densities of six different rocks/minerals collected from six different environments. Based on the brief description of each rock the students are asked to first predict which rock has the highest density and which rock has the lowest density. The students are then asked to construct a hypothesis and test their hypothesis by calculating the density of the rocks. Students are then asked to apply information from lecture to place each rock in the appropriate layer of the Earth.

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This module addresses the problem of how to determine the density of the earth and has students do some field experiments to get the data they need to answer the problem.

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This module addresses the problem of how to determine the size of a ton of rocks of a given composition and invites the student to figure out how to solve the problem.

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