The Greenland Subglacial Tremor Project started its work two years ago, planning logistics and travel for an expedition to Western Greenland. The field experience was delayed for two years due to the COVID-19 Pandemic. We finally deployed to Ilulissat, Greenland to study how glacier meltwater influences the speed and amount of ice flow and the rate
This PolarConnect event with teacher Erin Towns and researcher Dr. Sarah Das was broadcast live from Ilulissat, Greenland on 10 May 2022. The team was working on the Greenland Subglacial Tremor Project.
Jennifer Heidrich of the Warming and Removals in Mountains of Northern Canada expedition and Erin Towns of the Greenland Subglacial Tremor Project, have teamed up to create a podcast. Both educators teach at Edward Little High School in Auburn, Maine.
Sun Journal article coverage of two Edward Little High School teachers's, Jenn Heidrich and Erin Towns, both selected for PolarTREC expeditions. Jenn Heidrich was selected to go on an expedition in Yukon, Canada, and Erin Towns was selected to go on an expedition to Ilulissat, Greenland.
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
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