The core of the field trip began about 7 am on June 23.  Dr. Annexstad began with a story of how Lake Bemidji was used to test C130 cargo aircraft with skis to determine if they would work for landing on Antarctica.
 

Much of the trip between Bemidji and Grand Rapids was in a drainage way for the Wadena Lobe of the of the Wisconsinan glaciation period.  The remnants of the glaciation are the outwash sediments that form the topsoil, rivers and lakes of the region that are visible on the map.  So much water was released by the melting glacier that specific  channels were not established for some time forming  many valleys and braided streams in addition to the main channel that became the Mississippi River.  Today roadways are often built in or along these channels.  Some of the lakes that were left are called Oxbow Lakes as the drainage channel changed course and left behind a bend in the river that became a lake.   A basic review of glaciers and their cause by Steven Duch from the University of Wisconsin-Green Bay Illustrated Glossary of Alpine Glacial Landforms

   Further south and west is the Itasca Moraine (near Itasca State Park) that is material left over from the St. Louis Sublobe.   The vast majority of the surface of Minnesota contains only remnants of glaciers as the glacial sediments are up to 150 m (450 feet) thick. Only a few small areas have bedrock at or near the surface. ⁽¹⁾  The many bogs and lakes in the area are evidence of the relative youth of the system in comparison to the well defined drainage areas of southern Iowa and Kansas where there are very few lakes.

    This cross section bedrock map of Minnesota is a good resource to have handy throughout this virtual field trip. Looking at the small maps of the state (black) one should see a white line going from the north to the south with a slight angle to the east. As one lookes at the larger maps the bedrock indicated follows this line with the left side being the northern most part and the right the southern most part.

    The swamp or bog areas can be identified from the road by the lack of significant tree vegetation.  Where the ground is saturated with the water the vegetation is poor because of the lack of minerals in the soil.  Many areas have 40 to 50 feet of peat that has been deposited in the last 5000 years.  Peat is the precursor to coal and it is estimated that five to six feet of peat to get one foot of coal.  Wyoming  has some coal beds that are over 100 feet thick.

    By the time we get to the city of Deer River we are beginning to see outwash sediments from the St. Louis Sublobe which is still part of the Wisconsinan glacial period but occurred much later than the Wadena Lobe. We are in an area that has characteristic ground moraines or cover moraines that occur underneath stagnant ice.  The stones and rocks are well rounded and are mixed with silt and clay.

    At our first stop which is near the town of Taconite, we will see evidence of the mixture of material of the Wadena lobe that came from the north and the St. Louis Sublobe that came from the northeast.  This is near the edge of the glacial lake Upham and glacial lake Aitkin.  From Grand Rapids to Taconite we will cross gently rolling terrain that is the end moraines of the St. Louis Sublobes.  The material left by the glacier contains all kinds of unsorted sediment that is both rounded and angular.  Grand Rapids is also on the western edge of the Mesabi Iron Range that is defined by the Animikie Basin.
 

1.  Ojakangas, Richard W. & Matsch, Charles L.; Minnesota's Geology, 1982, p18