Valley Earthcache, CCARW10
Size:  (not chosen)
How Geocaching Works
Use of geocaching.com services is subject to the terms and conditions in our disclaimer
This cache has been placed for the CCARW10 event, held May 1-2, 2010. This cache was released to the public on April 29, but should not be located prior to noon, May 1. The caches for the event are released early so that the caching community has an opportunity to solve puzzles and plan their routes prior to the event start.
This cache has been placed as part of the Circle the Wagons class.
Most of Alberta’s rock and soil was laid down over 2 million years ago, and not much deposition has occurred since that time. The sandstone outcrop to the north east is known as the Paskapoo sandstone, and this formation was deposited about 60 million years ago. Take note of the limited depth of material above the sandstone. During the last 2 million years, there were several periods of glaciation that covered much of North American and Europe. Alberta was mostly immune to these periods of glaciation until the last major episode. During this last major ice age, known as the Wisconsin Glacial Episode, a sheet of ice covered most of Canada and northern Europe and Asia at thicknesses up to 4000 metres. Alberta was covered in ice up to 3000 metres thick with a sheet of ice known as the Laurentide Ice Sheet advancing from Hudson’s Bay, which was met in the west by the advancing Cordilleran ice sheet. Only some high mountains and parts of Cyprus Hills and Porcupine Hills escaped the ice. During this period, from 26,000 years ago until about 10,000 years ago, the world’s sea level fell by about 120 metres due to the water taken up in the glaciers. Much of the undulating terrain in Alberta and our drainage systems were created by the advancing and subsequent melting of these large sheets of ice.
Many valleys in Alberta were carved by the large volume of water running off the glacier to the sea. The volume of water flowing in our current streams and rivers is only a small fraction of the volume that was flowing during the melting of the ice. Some of the water would have flowed in incrementally large rates when large lakes forming on the top of the glacier suddenly broke through the edges of the glacier. It is speculated that some deep valleys in the mountains and elsewhere were formed within days when ice dams broke, suddenly releasing large floods of water, and deeply scouring the landscape with these releases. The steeply eroded valley to the north was created with the melt water draining the higher land to the north to the lower valley to the south. The valley you are looking at to the south and east was scoured by the advancing ice, and it would have been wet with the melt water 10,000 years ago when the melting ice sheets gave the nearby stream (Beddington Creek, passing under the bridge to the west of here) plenty of water for its source.
Both illustrations are from Natural Resources Canada
When the existing stream has a flow rate that is too low to have carved the valley in which it is contained, it is known as a misfit stream.
Please email us your estimates to the following questions:
1) How wide is Beddington Creek passing under the nearby bridge?
2) How wide is the valley at this location, and what is the elevation change from the top of the valley to the creek?
Please post your log after sending us your answers, and include a photo of the valley with your GPSr.
You may be interested in the other nearby caches that form part of this series of caches:
(No hints available.)
Loading Cache Logs...
Coordinates are in the WGS84 datum