Glacially Formed Features
Rivers
Bedrock
Glaciers
Random
100
This feature forms at the end of a continental glacier once its reached its maximum extension. 

Terminal Moraine

100

Where does the vast majority of erosion happen in a river? 

On the outsides of curves.
100

What is the MOHS hardness scale. 

Its a geologic tool that helps us categorize rocks by their apparent hardness. 
100

Tell me how a Glacier forms. 

During cooler climate periods, snowfall accumulates and doesn't melt annually. Over time, this builds pressure and compacts the snow turning it to glacial ice. 

100

What is Mr. Hackett's favorite hobby? 

Fishing

200

This feature is in the shape of a "spade" or "arrow head" and can tell you the direction a glacier moved even after its gone. 

Drumlin

200

Explain how erosion and deposition are linked in a river. 

Where ever there is erosion deposition will follow. 
200

Name a soft type of bedrock commonly found in Wisconsin (below a 4 on MOHS)

Shale, Limestone, Sandstone

200

How does a glacier get its movement? 

The accumulation center builds up and creates a slight slope. Gravity then allows the glacial ice to move away from the center. 

200

Name one of Mr. Hackett's siblings.

Isaac or Avery

300

These are groves carved into the bedrock where glaciers have traveled. They can also indicate the directionality of glacial movement.

Striations

300

What are two key features we can use to identify the direction a river will flow? 

The angle of the tributaries that flow into it. The width of the river from smaller to larger. 

300

Name a hard type of bedrock commonly found in Wisconsin (5 or above on MOHS)

Quartzite, Dolostone/Dolomite, Granite

300

What is the term used to describe the phenomenon that occurs when a continental glacier melts away and the Earth's crust responds by uplifting? 

Glacial Rebound

300

What is Mr. Hackett's wife's name? 

Anna
400

This glacial feature is the result of meltwater flowing over the top of a glacier and depositing in a conchoidal shape. Give the name of this feature and whether this feature will be made of sorted or unsorted materials. 

Kame, Sorted Materials

400

Give a general description of how the Wyalusing River changed into modern day Wisconsin River and Mississippi River. 

The Wyalusing River flowed through WI emptying into Green Bay. When the Green Bay lobe reached its maximum, it blocked the flow of the Wyalusing. This formed a lake which eventually overflowed. The overflow formed the new pathway of the Mississippi River and the reversed flow of the Wyalusing is now the Wisconsin River. 

400

What is the term for the phenomenon occurs when acid comes in contact with bedrock types containing calcium carbonate, causing it to bubble and produce carbon dioxide. 

Effervescence 

400

Explain why in Glacial Rebound Theory, why parts of the Earth's crust responds by increasing in elevation but other parts decrease. 

Because Earth's curst is connected. Like a paper cone, if you push the center up the sides will respond by going down. As the weight is lifted off the crust portions uplift where the majority of the continental ice was while the sides actually decrease in elevation. 
400

What is Mr. Hackett's go to sweet? Double points if you can guess the type

Donut

500

This is the large opening found in the top of a glacier created by excessive melt water that works its way down to bedrock. 

Moulin

500

What type of sediments would be found at the bottom of glacial meltwater lakes and why? 

Sand and smallest particles. Because they get carried furthest by water. 

500

Give me a summary of why the Bay of Green Bay is underwater and Door County is not. 

The Bay of Green Bay has a bedrock type consisting of a mix of Dolostone, Shale, and Limestone. Door County consists of harder pure Dolostone. Because of the many advancing and retreating of glaciers, the softer bedrock was carved out and the harder dolostone resisted erosion by glaciers more. 

500

Define the "Driftless Region" and tell me the major contributing factors to why/how it formed.

The "Driftless Region" is an area of Wisconsin, Minnesota, Iowa, and small part of Illinois that was unglaciated from the recent ice age. 

This occurred from the different hardness of bedrock and its locations in the midwest. Softer bedrock located to the North and East of Wisconsin allowed the glacial lobes to follow those pathways. 

Extremely hard bedrock in Wisconsin's North East slowed the advancement of the glacial lobes, with it stopping where the driftless region is located. 

Lastly, Lake Superior and Lake Michigan had bevels in their bedrock formations creating a lower elevation for the lobes to follow. 

500

Name the company Mr. Hackett used to work for before teaching. 

Cru