This lesson/project/lab has students predict via multiple drawings and time lapse photography predictive Flubber flow before the placement of barriers and other obstacles in front of the Flubber. Contour lines in two directions are drawn on both the paper prediction and the Flubber for comparison purposes.
Following predictive drawing completion glacier flow (Flubber flow), with obstacles in place
Ground penetrating radar is an important tool for studying glacier dynamics. Glacier scientists use GPR images to analyze attributes of glaciers. The following research activity will familiarize students with the basics of the different types of glaciers and their dynamics along with ground penetrating radar and its use in glacier studies.
Skidompha Public Library's Chats with Champions speaker program hosted well-known Nobleboro Central School teacher Ken Williams and his former student Seth Campbell at the library's Porter Meeting Hall at 2 PM on Saturday, January 11, 2014.
The two explained the unofficial title of their presentation: "Student finally hands in 1989 homework assignment to Nobleboro teacher at 14,000 feet in Denali
This activity was adapted from a TEA activity authored by:
* Sandra Kolb, Education Consultant, Poulsbo, Washington
* Kolene Krysl, Westside Community Schools, Omaha, Nebraska
* Larry Rose, Pleasanton Middle School, Pleasanton, California
* Wendy Slijk, La Costa Canyon High School, San Diego County, California
The original activity can be found at: http://tea.armadaproject.org/activity/kolb/tobesaltyseaiceornottobesaltyseaice_main.html
Students will independently explore the PolarTREC expeditions, and reflect on the scientific questions, discoveries, and outcomes of the work that is or has been done.
Description
Students will visit the PolarTREC website at www.polartrec.com, where they will find a teacher who is in the field presently, or was already in the field. You may select one expedition
This archive is from the Live from IPY! Event held May 1, 2008 with Emily Davenport and other researchers working aboard the USCGC Healy in the Bering Sea.
There were approximately 110 participants on the call.
Due to technical difficulties, there is no seperate audio file for this archive. We apologize for the inconvenience.
Students are presented with an actual series of tundra photos, which they use to develop a hypothesis for which sort of ground cover will have the most/least permafrost depth. Then they are given a set of actual data and use this to test their hypothesis
Objective
Students will:
* understand what permafrost is and how it develops
This lesson was modeled after some of the routine activities undertaken by the geologists on the Kuril Island Expedition.
Complete the following activities:
* Day 1 To measure a simple topographic profile with a level instrument or hand level and stadium rod.
* Day 2 To use the measurements from Day 1 (and/or actual measurements from the Kuril
This activity is designed to take place near or at the end of a unit on the ocean floor. Students should be familiar with the physical features of the ocean floor including the continental shelf, abyssal plain, seamounts and guyots, seafloor ridges and trenches, and submarine canyons. The students should have also previously learned about sonar methods for mapping the