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EarthCache

Houghton Lava Flow

A cache by DK Momma Send Message to Owner Message this owner
Hidden : 10/26/2011
In Michigan, United States
Difficulty:
1.5 out of 5
Terrain:
1 out of 5

Size: Size: not chosen (not chosen)

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Connection to the Earth Science Curriculum

Essential Question:

How can scientists make sense of the Earth’s history?

  

Earth Science Literacy Principles-
Big Idea 2- Earth is 4.6 billion years old.

Common misconceptions addressed when visiting this EarthCache

There is significant disagreement about earth’s age among scientists.

The Earth has always been pretty much the way it is now.

All rocks are more or less the same (a rock is a rock!)

 Michigan State Science Content Expectations Addressed:

·Grade 6

E.ST.06.31 Explain how rocks and fossils are used to understand the age and geological history of the Earth (timelines and relative dating, rock layers).


Key Earth Science/Geological Vocabulary Words-

joint: a fracture in rock along which there has been no displacement.                      

rift: a fault.

flow: a stream of molten or solidified lava.

basalt: a dark-colored fine-grained extrusive igneous rock.


Houghton Lava Flow

EarthCache

 This site which is behind a strip mall in the Keweenaw Peninsula provides a great opportunity to readily see volcanic flow from the Keweenaw Rift.

Coordinates- N47o06.686’ W088o35.084’

Michigan has ancient rock that dates over 3.5 billion years old that originated from tectonic plate collisions and eruptions from volcanoes.  This site is a fresh outcropping that was exposed through the building of the strip mall.  It is a great view of lava flow anatomy.  You can see where one flow begins and another ends.  Look for the bubbly top layer to connect with the dark bottom layer of the next flow.  The image below will help you to recognize where one flow begins and another ends.  Look for the contact points.

 

lavaflow

Figure 1.Lava flow. Anatomy of a lava flow.

 The Hawaiian Island lava flows are smooth at the surface and are called “pahoehoe”.  The lava flows in the Keweenaw also have a smooth surface.  These smooth surfaces of basalt contained bubbly (vesicles) areas that then filled up with minerals of various colors.

 Logging Q1: What different colors do you see in this lava flows surface?

 At this site, you also note there is more than one lava flow. You notice that the flows are not laying horizontal, but are on an angle. The top of the flow is a bilious green that is bubbly with the different mineral colors in the bubbles.  The bottom portion of the flow is a black color.  Find the top of a lava flow.

     image 2

Figure 2. Houghton Lava Flow. MiTEP participants viewing the Houghton Lava Flows. 

 Logging Q2: How do you know where one flow begins and one ends?

 Logging Q3: How many lava flows are there?

 

Reference and Citations-

Jenkins, J. (photographer). (2011). Houghton Lava Flow (Image). Retrieved July 25, 2011.

Rose, W. (Instructor). (2011). Anatomy of a Lava Flow (Image). Retrieved July 25, 2011 from: http://www.geo.mtu.edu/~raman/SilverI/MiTEP_ESI-1/LavaFlowTops.html

 Schaetzl, R.; Darden, J.; Brandt, D.  (2009)  Michigan Geography and Geology.

New York, New York. Pearson Custom Publishing.


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Current Time:
Last Updated: on 11/15/2017 3:47:32 PM (UTC-08:00) Pacific Time (US & Canada) (11:47 PM GMT)
Rendered From:Unknown
Coordinates are in the WGS84 datum

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