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Journals 2006/2007

Miriam Sutton
Newport Middle School, Newport, NC

"Study of the seafloor and shallow subseafloor off the Labrador Shelf and Slope"
Canadian Coast Guard Ship Hudson (CCGS Hudson)
August 5 - September 1, 2006
Journal Index:
August 5 - 6 - 7 - 8 - 9 - 10 - 11 - 12
         13 - 14 - 15 - 16 - 17 - 18 - 19
         20 - 21 - 22 - 23 - 24 - 25 - 26
         27 - 28 - 29 - 30 - 31
September 1

Additional Resources

August 25, 2006

August 25, 2006 It's the Law

AM Location: Slope off Saglek Bank (58° 14' 21.27" N, 59° 42' 36.10" W)
PM Location: Slope off Nain Bank (58° 13' 07.69" N, 59° 11' 42.54" W)
Sea Temperature: 5.1° C
Air Temperature: 5.7° C
Hydrospheric Conditions: The seas continued to build through the night, increasing to 2 - 3 meter heights with choppy tops for the duration of the day
Atmospheric Conditions: Fog dissipated by morning but the cloudy skies persistently battled the sun throughout the day
Wind Speed/Direction: 30 knots/NE switched to 20 knots/NW

I ventured into the Core Storage Bin this morning to take a closer look at the sediment cores and the process used to preserve them until the scientists can return to the lab at the Bedford Institute of Oceanography in Halifax, Nova Scotia. Each section of the core is coded and stored top side up, in the same position that it was retrieved from the seabed. This positioning also assists the scientists in applying one of the key laws of geologic science: The Law of Superposition. This law states that in undisturbed layers of sediment (or rock), the younger layers lie on top of the older layers. (See Cross-section illustrations below.)

Cross section of seafloor sediment layers and a core sample

The diagram on the left illustrates a cross-sectional view of the seafloor sediment as it piles up along older layers that lie beneath the younger layers that are deposited toward the top. The cores collected provide the scientists with an even smaller cross-sectional view of the sediment layers. Some of the cores collected by the scientists contain mud and sediment from as far back as the last Ice Age, over 10,000 years ago. (See Core Storage photo below.)

Sediment Cores Stored at 4° C (Photo: Miriam Sutton)

Today's Activity: Use a shovel to pierce a section of compacted dirt in your yard. Try to insert the shovel as straight as you can through the top layers of soil. Insert the shovel between 8 and 10 inches deep into the ground and then pull the shovel toward you to reveal the different layers of sediment that have been deposited over the past several weeks or months. Observe and count as many different layers of sediment as you can. An alternative to this activity is to dig your shovel into the hard-packed sand the next time you're at the beach and observe the various layers left by the tides and waves along the seashore.

Word of the Day: Ice Age

REMINDER: Record today's Sea Surface Temperature (SST) and the Air Temperature on the data table you created from the August 05 journal entry.