Do you think she’ll start? While surveying harvest blocks in the Marten Hills by Slave Lake, we found an old car parked on the side of an old overgrown road. While not as unique an old plane crash, it does show how much an area can change. What used to be a road is now an overgrown trail through the forest.
Archaeology is messy work, but sometimes things get really wet and muddy! Elenore and Teresa are practicing here what is called “wet screening.” Wet screening is similar to dry screening as you try to get all the sediment through a mesh screen, but water is used to wash away any particularly thick lumps of sediment. Once all the dirt has been washed through the screen, any rocks or artifacts will be left behind to find. This is a particularly effective way of dealing with heavy clay or bulk soil samples, but requires a lot of water and a place that you don’t mind getting messy!
Welcome to a snowy day in the Swan Hills! We found a small archaeological site on this point, overlooking this big beaver pond which had just started to freeze over. It was a long hike through swamp and snow to get to this place, but it was worth it!
Ever wonder what happens to that balloon that slipped from your fingers as a kid? What goes up must come down. This particular happy birthday balloon was found 30 km from the closest town, but it probably came from much further away. It wasn’t Matt’s birthday, but it did bring some much needed entertainment to the day!
Where we find archaeological sites in the province is often strongly tied to the physical environment. We look for the different physical characteristics such as distance to water and if an area is high and dry. These features are indicators, which tell us that there could be an archaeological site in the area. This approach to finding archaeological sites is useful, but there are problems when we start considering how the landscape might change over time. The top of a hill set really far from a stream today, might have been beach front property in the past.
This is important in regards to our work on the shores of Lesser Slave Lake in Alberta. The Lesser Slave Lake basin has undergone extensive changes over the past 13,000 years, largely due to the retreating front of the glacial ice sheets at the end of the last ice age, and the incision and creation of the modern river valleys. Understanding how this environment changed over time is useful for identifying new archaeological sites in the region, as it helps us to understand how First Nations used the landscape in the past. Older archaeological sites may be on ancient beaches and meltwater channels that don’t look like they would be suitable for a campsite today, but were actually prime real estate 10, 000 years ago. These sites could be missed during an archaeological review and survey based on the modern landscape, so it is important that we understand how an area has changed, so that we can better predict where archaeological sites are going to be.
Over the past few weeks, we’ve seen a lot of rain hit areas of the province. During this time of year, the hot humid weather generates plenty of late afternoon thunderstorms. These storms can blow in quickly with heavy rain, leaving you drenched to the bone. Just one of the many fun challenges of working in the forests of Alberta. It does lead to great photo opportunities like this one. This photo was taken on the north shores of Lesser Slave Lake, while a intense storm was sweeping through the south shores of the lake.
Check out Brian Leslie looking very thoughtful near Slave Lake, Alberta