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Last modified:
June 4, 2009
What is a Crackmeter?
Crackmeters (or crack gauges) are installed within the large cracks on the mountain peak. These instruments are thin steel rods anchored on both sides of the crack wall and measure how the cracks pull apart in relation to slope movements. The most sensitive of the different monitoring systems is a vibrating-wire crack gauge (crackmeter) that can detect changes as small as ten microns - the thickness of a human hair.
On Turtle Mountain, 22 active crackmeters have been installed in
accessible areas on the western side of the south peak. At six locations,
the crackmeters were installed in sets of three and placed at different
angles across the crack. These orientations allow for detection of the
true direction and magnitude (vector) of the movement at the monitoring
location.
The ends of a crackmeter are fixed into 12.5 mm (3/8") holes drilled into the sides of the fissure. The length (including extension rods) is approximately one metre. The cabling runs through flexible conduit back to the datalogger at the weather station, where data are recorded and stored until telemetered back to the Frank Slide Interpretive Centre.
Readings are taken every 15 seconds and averaged once an hour before transmitted to the data centre at the Frank Slide Interpretive Centre.
Overall, the crackmeters have functioned reliably since their initial installation in the fall of 2003, but there were some negative effects from snow and ice on the instruments. Although we built metal roofs over the crackmeters to protect them from snow, the combination of blowing wind and snow caused snow and ice to accumulate underneath the housing and on the crackmeter rods. This caused significant damage to the instruments and required annual repair and maintenance. In summer 2007, we upgraded the roofs and didn't notice any snow accumulation issues during the winter.
Through monitoring, we have noticed a consistent width change of the cracks each year due to temperature changes. In the spring and summer, the rock expands, making the cracks narrower. In the fall and winter, the rock contracts, causing the cracks to become wider.
We have measured width changes of approximately 0.4 mm during each cycle. Total crack widths range between 1 and 1.5 metres at the crackmeter locations. Daily temperature changes have also caused width changes (around 0.02 mm); however, we have not recorded a permanent change after every cycle. Electrical noise has caused alternating changes up to 1.5 mm as shown below. We believe this is from lightning strikes.
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