BCC Bioscience Image Library is a media file repository of images and video clips made freely available to the public, with special attention to the needs of educators and students in the biological sciences. The resources are licensed under Creative Commons 0. This means all content is free, with no restrictions on how the material may be used, reused, adapted or modified for any purposes, without restriction under copyright or database law.

This project was partially funded by a $20,000,000 grant awarded by the U.S. Department of Labor’s Employment and Training Administration, Grant # TC-26450-14-60-A-25. The product was created by the grantee and does not necessarily reflect the official position of the U.S. Department of Labor. The U.S. Department of Labor makes no guarantees, warranties, or assurances of any kind, express or implied, with respect to such information, including any information on linked sites and including, but not limited to, accuracy of the information or its completeness, timeliness, usefulness, adequacy, continued availability, or ownership.

If you have any questions contact professor Faye Reynolds at: bioimagesoer@gmail.com

During the course of the day, students examine the high-grade metasupracrustal rocks, related gneisses, and the late Archean granitoids and mafic dikes. We have prepared a number of exercises that might be done with classes at different levels. Depending on the background and preparation of your class you might want to emphasize different learning skills specific to the class level: observation, interpretation, integration (i.e. multiple lines of evidence focused on a given problem), and synthesis (i.e. relationship to the "big picture", drawing from the corpus of geologic knowledge). We have also prepared a compilation of our key scientific results, but these are under seal and we'd like you to do the exercises first as if you were students before taking a look at the supporting evidence.

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To prepare for this activity, students receive background on bedforms and flow regimes in class and practice identifying and classifying bedforms from field photographs. Students are then given a map of a barrier beach/inlet/tidal delta complex in mid-coast Maine and asked to predict what bedforms they expect to find in specific sub-environments. During a subsequent field trip to the area, students observe, classify and map bedforms and relate them qualitatively to formative flows. Qualitative description and classification are supplemented by quantitative measurements of bedform morphology and orientation, and by GPS-located digital photographs. After the trip, students compare their predictions and observations of bedforms in the sub-environments, reflecting on the reasons for the differences and the evolution of their thinking. The exercise also serves to set the stage for subsequent quantitative studies of bedforms and bedload transport, as well as interpretation of sedimentary structures and clastic depositional environments in the geological record.

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This module presents some of the general ideas behind and basics principles of high-performance computing (HPC) as performed on a supercomputer. These concepts should remain valid even as the technical specification of the latest machines continually change. Although this material is aimed at HPC supercomputers, if history be a guide, present HPC hardware and software become desktop machines in less than a decade.

Biodiversity is a useful measure to help us understand the range of diverse species that make up our ecosystems! Calculating Species Diversity is an interactive tutorial that walks learners through the different types of species diversity and how to calculate them. Additionally, learners will gain an understanding on how human activities negatively impact biodiversity and how they can help alleviate the side effects of these actions.

Cancer is an everyday topic in the news and in most extended families. The types and treatment of cancers can be complex and confusing. Module 2 provides students with knowledge and resources concerning the development of cancers related to environmental factors. It is important for students to realize that the state-of-the-art of cancer treatment prior to 1986 (the year the trial started) is not the current state-of-the-art. Treatment of many types of cancer has progressed enormously due to medical research. Treatment of childhood leukemia is one of the success stories in cancer treatment. Research linking childhood leukemia to environmental factors or a specific environmental factor has progressed more slowly. Several links are provided within the website that students can read to become aware of environmental factors in Woburn that have been studied, including Woburn Chemical Industry, Woburn's Water Supply and Hematology of Leukemia. Several research articles are available for students to read and are cited within the searchable database at Bibliography & References.

This tombstone weathering lab is designed to provide students with tangible understanding of chemical weathering and weathering rates. To prepare for this lab, students will have learned in previous labs to identify common minerals and rocks and will have attended lectures about the process of chemical weathering. During the first part of the lab we travel to the city cemetery to collect data on the age and extent of chemical weathering of tombstones that are made of limestone and igneous rocks. After collecting data for ~1 hour, we return to the computer lab where students use Microsoft Excel to analyze and interpret their data. Their task is to calculate a chemical weathering rate for limestone for our region and compare that rate to those from other regions. This activity gives students experience in the process of scientific inquiry: data collection, data analysis and data interpretation. Students develop Microsoft Excel skills: writing formulas, producing charts, understanding trendlines and R2 values.

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This transect across northern Washington State was one of our most geologically and biologically diverse field trips. The trip started with a drive across the relatively uniform basalt flows of the Columbia plateau and then traversed the extremely geologically complex North Cascades accessible from a scenic route through the small, and relatively less-traveled, North Cascades National Park. Steep gradients in elevation annual precipitation and winter temperatures revealed equally dramatic changes in vegetation from cold desert shrub lands to temperate coastal rain forests. Like previous trips, this one allowed students to observe glacial processes up close and trace the history of plant succession as glaciers retreat.

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This trip followed the Columbia River across the basalt flows of the Columbia Plateau through the Columbia Gorge that bisects the Cascade Range and then turned south along Oregons spectacular coastline. The opportunities to integrate biology and geologic processes were limited only by time as students explored the plant and animal life of rocky and sandy beaches dune fields and coastal forests. The southernmost portion of the trip extended from Crescent City, CA (site of the 1964 tsunami) through the Klamath Mountains on the Oregon/California boundary one of the most geologically dynamic landscapes in North America. The tectonic history of the region with its resulting shifts in climate patterns and merging of previously isolated land forms along with an unusual abundance of ultramafic rocks have driven the evolution of one of the most diverse floras in North American populations of carnivorous Darlingtonia (Pitcher plants) provided a dramatic example of the unusually large number of plant species endemic to the serpentine soils of this region.

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This project involves a field trip to the Jordan Formation in Winona, MN. Student teams are assigned a section of the outcrop from which they are to determine a stratigraphic column. The class then performs a lateral analysis and builds a composite stratigraphic column for the formation. As a final product, the students write up the class's observations about the formation.

Project Webpages

Project Summary and Write-up Outline (Acrobat (PDF) PRIVATE FILE 115kB Jul7 05)
Instructor Notes for Project (Acrobat (PDF) PRIVATE FILE 91kB Jul7 05)
Outlines and Notes (Acrobat (PDF) PRIVATE FILE 1.1MB Jul7 05) for each class session for this project

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The processes of conducting a deposition and developing strategies for being deposed or taking depositions are described in this module. The webpages herein reference to The Federal Rules of Evidence and excerpts from the actual depositions of various experts in the Woburn Toxic Trial including John Drobinski, George Pinder, John Guswa, and others. This module describes the setting for taking depositions, how attorneys slowly extract information from those being deposed, and the typical proceedings during deposition. This module can be a stand alone, but the information is best coupled with the modules where students prepare court exhibits to augment and display their technical arguments. This module stresses the need for clarity and parsimony when presenting technical arguments with opposing counsel.

This unit provides pre-service teachers in methods courses with resources for teaching geoscience content and utilizing the methods of geoscience. Pre-service teachers will prepare an annotated bibliography of instructional resources in the areas of geology, meteorology/climatology, oceanography, and astronomy. They will select one of these resources and prepare a full lesson plan based on the resource that emphasizes the methods of geoscience and also incorporates interdisciplinary material from either biology, chemistry, physics, or the social sciences.

This module introduces students to the fundamental principles and uses of electrical resistivity, with a focus on an environmental application. Students explore the characteristics and environmental setting of Harrier Meadow, a saltmarsh just outside of New York City. They investigate the relationship between electrical resistivity and physical properties of the soil in the marsh. Students also discover how variations in survey configuration parameters control investigation depth (how far into the ground the signals sense) and spatial resolution (what size objects can be detected). Finally, students learn about and then perform geophysical inversion, which is the process of estimating the geophysical properties of the subsurface from geophysical observations. In the final unit of the module, students evaluate the extent to which the geophysical dataset and direct physical measurements support the hypothesis, introduced in Unit 1, accounting for the distribution of Pickleweed in Harrier Meadow.
This module is intended to require approximately 2-3 weeks of class time. Teaching material includes PowerPoints that may be used in lectures or provided for self-guided learning, exercises, and handouts that ask students to synthesize what they learn from the exercises. In addition, multiple choice and short answer questions can be given to students as homework, on quizzes, or on exams.

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Testimony by expert witnesses is unique in a trial because qualified experts can present opinions as testimony, rather than merely stating implicit facts. This module links users to the Federal Rules of Evidence so they can view and interpret the rules regarding qualifying an expert. In addition to the definition of an expert witness, which is referenced in Article X of the Federal Rules of Evidence, information regarding trial exhibits and the form of trial exhibits are included. Links to mock trial videos are provided so that participants in a mock trial can view the courtroom arrangement and determine how to best utilize exhibits in the courtroom and in the mock trial.

Ithaca NY is currently located in a tranquil mid-continental geologic setting. But Ithaca's past was anything but tranquil. Would you believe that we once sat beneath a mile-thick sheet of ice? Or that it was once the bottom of the ocean? In a zone of high seismic activity? Or volcanic eruptions? It's all true. On this field trip to Enfield Glen, in Upper Treman State Park, we will make measurements and observations that allow us to reconstruct some of the events in the geologic past of this locality. Was New York always on the east coast of North America? Come on, let's find out.

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In-service teachers learn about environmental geology and how to teach earth science using outdoor activities and resources near their schools.

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Members of the Department of Atmospheric Sciences at the University of Illinois Urbana-Champaign have designed a suite of atmospheric science learning modules for middle school students. The curriculum, which implements a flipped-classroom model, is cross-referenced with Common Core and Next Generation Science Standards. It introduces students to topics such as temperature, pressure, severe weather safety, climate change, and air pollution through short instructional videos and critical thinking activities. A goal of this project is to provide middle school science educators with resources to teach while fostering early development of math and science literacy. The work is funded by a National Science Foundation CAREER award. For a complete list of learning modules and to learn more about the curriculum, visit https://www.atmos.illinois.edu/~nriemer/education.html

This is a 10-day field experience class that focuses on the geology of the Grand Staircase of the Colorado Plateau, culminating in a rim-to-rim backpack trip across the Grand Canyon, Arizona.

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This activity introduces geoscientific thinking to a primarily non-geoscience audience. This is the introductory activity of a module designed for pre-service secondary science teachers in a secondary science teaching methods course. Initially, students explore their conceptions of the scientific method. Through readings and discussion, the activity attempts to broaden the students' view of the nature of science by showing how geoscience methods differ from stereotypical experimental science. This introductory activity uses a seminar format (writing/reading/discussing/writing).

The flow or discharge value in a river does not mean much to a lay person or a decision maker because this flow can be insignificant on a big river or can be dangerous on a small creek. Thus, we must know how to translate this flow value into the water depth, velocity, and the corresponding extent to understand its impact. The objective of this unit is to perform hydraulic modeling on a reach of Wabash River near Lafayette, Indiana, to estimate water surface elevation and extent corresponding to a 100 year flow. Students will learn the basics of hydraulic modeling using HEC-RAS to simulate the flow hydraulics using one-dimensional steady state assumption. The outcome will be the inundation extent corresponding to the 100-year event along the reach of the Wabash River near Lafayette, IN. Make sure you have HEC-RAS available on school or personal computers prior to the start of the unit.