ISS015-E-7649 Click the photo number to access all resolutions available and the database record.
The velocity of Saskatchewan River slows significantly as the river enters Cedar Lake; as the velocity slows, silt, clay, sand, and gravel are deposited at the river mouth. These deposits (light tan and gray in the image), called alluvium by geologists, border the active channels of the Saskatchewan and Summerberry Rivers.
As the deposits accumulate, they impede the river’s flow. Old channels are abandoned, and new ones form as the river seeks an easier path into the lake. Through this process (known as avulsion), the delta builds and branches out over time. A typical “bird’s foot”-shaped delta is currently forming at the mouth of the Saskatchewan River (image lower right). The bird’s-foot structure is approximately 13 kilometers wide. The Mississippi River’s active delta has the same general form, but it is much larger—approximately 50 kilometers wide.
The bogs in the Saskatchewan delta are saturated enough that peat (dead plant material that accumulates in a water-saturated environment) has formed. Over long periods of time and under the right geological conditions, peat deposits can become coal. The accumulation of plant and animal remains in the water-logged, oxygen-poor environment greatly slows down decay. In addition to setting the stage for coal formation, these conditions also preserve fossils of many kinds. The delta sediments at Cedar Lake are a rich source of fossil-bearing amber that was preserved along with coal deposits during the Late Cretaceous (about 65–99 million years ago). These deposits were not formed locally, however; they have washed into the delta from coal deposits over a thousand kilometers to the west of Cedar Lake.
