Last year I visited a very interesting site located near Canmore, AB. The Rat’s Nest Cave is accessible through the touring company, Canmore Cave Tours, and can be visited all year round. With the help of my guide, Brent, I rappelled 18 m into the cave and squeezed through many tight water carved gaps and tunnels. Eventually you reach “the grotto” where you can hang out by a crystal clear pool and several beautiful stalagmites and stalactites.
Also in the cave are many animal bones dating to approximately 7000 years ago and, although I didn’t see any while on the tour, several stone tools dating to 3000 years ago. One of the most fascinating aspects of the cave are the pictographs located at the entrance of the cave. Inside the cave, are several small rock paintings that indicate the cave was of cultural significance for the First Nations people possibly for thousands of years. My guide also informed me that there are several pictographs on the outside of the cave above the entrance but due to years of weathering they are not visible to the naked eye.
Luckily, recent advances in technology allow us to digitally enhance rock art paintings. A process called Decorrelation Stretch or simply D-Stretch is currently being used by archaeologists and rock art researchers to enhance even the faintest of pictographs. The process works by increasing differences in hue and stretching the contrast for each colour variance. When D-stretch is used to enhance the image of the entrance of the Rat’s Nest Cave, a series of handprints can be seen going up the wall.
Anyone that works all day in the wilderness knows the importance of having a quality piece of Load Bearing Equipment (LBE) that accommodates all the odds and ends that are required of your profession, while being comfortable enough to wear for prolonged periods. LBE comes in a variety of styles, from the standard Cruise Vest, to the more tacticool modular equipment based off military style plate carries and H-harnesses that employ MOLLE attachment systems. Archaeologists at Tree Time Services Inc. have tried and tested a whole gambit of systems over the years, and everyone but a few outliers (Reid loves his cruise vest), have adopted the True North Aero Vest – Wildland as our LBE of choice.
Before I start the review section, there is one important aspect of our job that influences what type of LBE we prefer. We need to carry more gear than can be accommodated by LBE alone, so that a good backpack (30-50 Litre) is a necessity. Even though some people have tried to fit all the required equipment in their cruise vest, you can only fit the bare minimum of what we need to bring, and have to abandon some items that aren’t necessarily required, but are extremely valuable in certain situations. Things like rain gear, extra thermal layers, extra socks, survival kits, extra food and extra water will not easily fit in a cruise vest when it is filled with all the items that are required for archaeological survey in the boreal forest. Also, if you do try to fit all those things in your cruise vest, you will no longer be able to work effectively while wearing it. Furthermore, attaching your screen to your backpack with a bungie cord is arguably the best way to carry your screen for long hikes, and allows you to stow things such as a hoodie or jacket between the screen and backpack. For these reasons, almost every archaeologist at TTSI uses a combination of some type of LBE and a backpack.
The Cruise Vest
Cruise vests have been around for a long time, are widely available, and come in a variety of colour and materials. In my opinion, they are fine if your profession requires you to be mobile in the field and your profession does not require much equipment. Reid uses a cruise vest made from a plastic mesh and considers this to the best vest as it is durable and breathable. Cruise vests can be expensive ($100+), and even more so if they have an internal frame. Yet they still don’t accommodate all the extra gear needed for adverse conditions. Teresa and Tim have both used the cruise vest with internal backpack frame, but Teresa has since switched to the True North Aero and hasn’t looked back.
Comfortable if not carrying much equipment
Variety of colours and fabrics
Cons (With no backpack feature)
Not enough storage space
Very uncomfortable when overloaded
Very uncomfortable while riding ATV
Cannot wear while digging
Secondary HiVis still needed
Bad screen attachment
Cons (With backpack feature)
Less gear retention
Uncomfortable with backpack
Full pockets impede pack waist straps
Not adjustable for winter layers
Flimsy and wear out quickly
Non-breathable and hot
The Modular Vest
Modular vests have been around since the 1990’s and have generally replaced what was typically referred to as “web gear” by many Armed Forces groups around the world. They employ a Pouch Attachment Ladder System (PALS), also referred to as MOLLE, which allows the user to change what types of pouches they use based on personal needs without changing the base vest. Most modular vests also act as plate carriers (body armour) and allow the user to change their load-out while still utilizing their body armour as a base. Although modular vests are widely available, most are in neutral colours or camoflage and are therefore not suited to working with a HiVis requirement. With hunters in mind, a few companies have produced modular vests that are blaze orange, and thus work as HiVis provided the rules concerning HiVis clothing are not super strict (some companies would not consider any of these options to be sufficient HiVis clothing). Kurt used a modular vest for a couple field seasons, but has since switched to the True North Aero. He provided the following list of pros and cons:
Modular and adaptable
Can wear while digging
Very adjustable and can fit winter layers
Most are not HiVis
Non-breathable and hot
Not comfortable with backpacks
True North Aero – Wildland
True North is a company that primarily produces gear for Wildland Fire Fighters and First Responders. The True North Aero was designed as a primary piece of LBE that could be worn comfortably with a backpack. Although True North makes specific products that compliment the Aero, we at TTSI have found that this particular LBE to work with a variety of backpacks. The Aero has a specific spot for radios, GPS, flagging, tape measure and has a fleece lined pocket that fits a iPad Mini perfectly. Essentially, the Aero can accommodate all the equipment need while actually working, and in conjunction with a 30-50 L backpack, provides all the space you will ever need. A further benefit of using the Aero in conjunction with a backpack is that since all your survey equipment fits in the vest, one does not have to unpack their backpack to survey a target. Kurt was able to obtain several Aero vest in blaze orange, but unfortunately they seem to have discontinued so only the black version is widely available. While wearing the black version, TTSI employees usually opt to wear a HiVis work shirt.
Comfortable to wear with backpacks
Breathable and cool
Fits all survey equipment
Holds gear secure
Can wear while digging
Protected inner fleece pockets
Few zippers, but high quality
Sheds water and dries out fast
Very adjustable and can fit over winter layers
Not true HighVis
Zippers can get clogged with mud
There are many options when it comes to LBE and like most things, not everyone will agree on what is the best. Reid stands fast as a die hard proponent of the mesh style cruise vest as it is durable, breathable and works well with his system. Similarly, Tim continues to use the internal frame cruise vest even though he has had the option to switch. However, the rest of us archaeologists at TTSI have chosen the True North – Aero as our LBE champion and never looked back. I personally think it will be a very sad day when my blaze orange version finally wears out and I am unable to get a replacement. On that day, I will regrettably don a HiVis undershirt, strap on a black True North – Aero and head off into the boreal wilderness.
In 2015 a two year poll was issued by Canadian Geographic for a new National Bird. In the end, our little Grey Jay took the lead, beating out the common loon, black-capped chickadee, snowy owl, and Canadian Goose. Although not officially recognized as the new National bird yet, it was selected as an avian representation of Canadians: its found in every province and territory, it’s friendly, and it’s very intelligent!
For the Cree, the Whiskey Jack, or Wisakedjak, is a shape-shifter, benevolent trickster, teacher, and messenger of the forest. There are many different stories about the Wisakedjak, but most of them have a moral. The appearance of the Wisakedjak in the morning is seen as a good omen, and is believed it warns people of nearby predators.
This boreal forest inhabitant is often spotted by Tree Time’s archaeology crews, and it has quickly become my favourite little bird. They are almost always seen traveling in a group of three: a monogamous pair and a juvenile from the previous year’s breeding season. The friendliest groups have always been found near areas people have made their hunting camps. In fact, the Whiskey Jack has figured out that people mean food. Given a few minutes, some of them may even eat out of your hand!
Whiskey Jacks stick around all winter too, even incubating their eggs as temperatures dip to -30°C. They store their food in crevices, under lichen, and even under conifer needles. They coat the food in a saliva, called bolus, which makes it sticky, ensuring the food doesn’t move until the Whiskey Jack returns. Unlike forgetful squirrels, these birds will remember exactly where they left their caches! Their food is a variety of arthropods (like spiders), small mammals, ticks, carrion, fungi, fruits, and seeds. The average life span is about 8 years, although the oldest recorded Whiskey Jack was 17 years old!
During our field seasons we find 100+ archaeological sites every year; however, not every site we find is flagged for avoidance. The decision of whether a site is avoided or approved for impact ultimately comes down to the Historic Resource Management Branch at Alberta Culture and Tourism’s approval of our recommendations. Our recommendations are based on the following criteria of site significance:
Multiple Component: The continued use of a landform throughout time increases the site significance. This can be represented by stone artifacts from different, distinct depths or in different layers. The most obvious multi-component sites are historic period sites (Post-European Contact) with an earlier Pre-European contact component. For example, we have found stone tools in tests conducted around the outside of a collapsed cabins.
Integrity: Sometimes we assess areas after they have been disturbed. We do this either to assess the level of impacts from the disturbance or protect sites from any further impacts (site preparation for tree planting, gravel pits, etc.). If we believe the site has been completely disturbed and the artifacts have lost their context, we will collect a representative sample of artifacts and recommend approval for the impacted area.
Road exposure with artifact identified
Artifact found in disturbed context
Biface fragment of artifact found above (dorsal – left, ventral – right)
Datable Materials: The presence of organic material is necessary to determine how old the site is. This is quite rare in the boreal forests of Alberta because the acidic soils do not preserve things such as bone or wood. Often, the only datable material we find is charcoal which can be used for Carbon dating. The ability to date the site is important as archaeologists are still figuring out the evolution of tool use and the spread of people throughout Alberta.
Thick charcoal deposits from a shovel test
large pieces of charcoal are required for dating
results of radio carbon dating
Exotic Materials: The sites we find are typically scatters of tool stone such as quartzite and chert. These materials were local to the area, collected from stream beds by the past flintknappers. When we find something not native to Alberta, we consider the site to be of high significance. The presence of obsidian suggests trade or travel from areas with volcanoes. The presence of Knife River Flint suggests trade or travel from North Dakota.
Presence of tools or diagnostic materials: The majority of sites we find are simply areas where a stone tool was made. To find a tool is significant because it tells us what activities were happening at the site. These tools can include things such as: scrapers for scraping hides; knives for butchering animals; wedges or adzes for woodworking; or projectile points (e.g. arrowheads) used for hunting. Projectile points can also be diagnostic of certain groups (e.g. Clovis) or certain time periods (e.g. spears>darts>arrowheads).
Distinct intra-site activity areas or features: Sometimes we can find things that suggest a certain activity happened at a specific area of a site. This can be represented by what we call features which are non-portable representations of human activity. These can be such things as: post holes, hearths, or walls. We can also find distinct activity areas such as the flake scatter identified at the Brazeau Reservoir.
Uniqueness of the site in the surrounding area: We often find ourselves in areas of the province that have never had an archaeological survey before. I’ve found sites in areas of the province that we would describe as “the middle of nowhere.” Basically areas that are from major rivers or known travel corridors that were used by people in the past. To find a small scatter of flakes in an area without another site for another 20 km in any direction is more significant than finding another site in densely occupied areas such as the Fort McMurray region.
Site size: Our work is primarily concerned with determining how large the site is for purposes of avoidance by our clients. When we find very large sites these are considered of high significance due to the increased potential of finding anything listed above.
Back in September of 2017, I found what would probably be one of the coolest artifacts that I will ever find in my field survey career. My coworker Vince and I got up one fateful morning and set out on our four hour quad ride into one of the most beautiful areas in Northern Alberta: the Swan Hills. I have been working in the Swan Hills area for a few years now and every time I come back, I am always amazed by the broad vistas and pristine valleys that cut through this segment of the Alberta Foothills.
We were checking out a cutblock on the edge of a broad muskeg flat with a small stream. It was pretty swampy on the way in, but once we got closer to the stream, the land rose up into a nice, narrow little ridge that gave a good view over the stream. After walking around for a bit, Vince and I settled on a place to start digging. Normally, it takes a bit of time going through the screen before you can find the small stone flakes that we typically find. This time, I only had to flip over the root mat to see the top half of a stone blade stuck in the rootlets. A few seconds later, I pulled out the base of the same blade from the loose sediment, revealing a complete spear point buried only a few centimeters below the surface.
You can only imagine my excitement once I pulled this beautiful specimen out of the ground (I think I was making noises akin to Homer Simpson drooling over a doughnut). It is hard enough to find artifacts in the Boreal Forest, let alone to find a tool! My first thought as soon as I pulled it out was that I had found an Alberta Point. This is a type of projectile point that dates to around 9500 and 8000 years ago and is part of what is known as the Cody Complex. Alberta Points commonly have square stems that would have been hafted into a spear shaft, along with broad distinct shoulders and wider tapered blades. It seemed to be a good fit for the style of the point that I had found so I put Alberta Point in my notes and went about my day.
Back at the lab, I started flipping through my reference books. I began to realize that what I had found didn’t really fit with what we know about Alberta Points. The shoulders weren’t as square as other Alberta Points and the blade was a little too broad and less lance-like. I also noticed that the shape of the point closely resemble ones found at Hell Gap sites, dating to between 10,000 and 9,000 years ago (before the Alberta points and the Cody Complex). During this period, we see that First Nations ancestors were making similar large spear heads, but with a broader blade and slight, indistinct shoulders. So the spearhead that I found could also belong to this time period. However, the story doesn’t end there. To complicate matters more, there are also similar kinds of projectile points being made around Lake Athabasca in the northeast corner of the province. During the Early Taltheilei Phase (2600 to 1800 years ago), the caribou hunting people living on the shores of Lake Athabasca were making similar looking large spear and atlatl dart points. The point I found could fit into any one of these three possibilities.
So what kind of projectile point had I found? If we can identify the style, we can make inferences on the age and archaeological culture that was present at the site. Being able to place an age on a site is often difficult to do for Alberta sites, especially sites in the Boreal Forest. The lack of organic preservation at many sites means that radiocarbon dating is often not possible. Also, most archaeological sites in northern Alberta have very little stratigraphy, meaning that you will find 13,000 years of history in about 20 cm of soil. Even this artifact, which may be anywhere from over 10,000 to 2000 years old, was found only 5 cm below the surface. So if I were to determine how old this site was, I would need to be able to positively identify the type of projectile point that I had found. So what did I find? How was it made? Where did it come from? The answers to these questions can tell us about the people who made the artifact.
First off, the material. The point is made of fine-grained quartzite, a lithic raw material that was frequently used in Alberta all throughout history. There are a lot of advantages to working with quartzite. As a material it is very strong and durable, which means that the edge of the blade will hold longer than other materials like obsidian. This also means that it is extremely difficult to work with. When we try our hand at flintknapping today, we often start with obsidian, chert, or flint because these materials will fracture more easily and predictably than others. Pick up a raw quartzite cobble, and you’ll find that you be bruised from trying to crack it open.
Quartzite is also very common. Almost every stream, creek, and river valley is filled with a variety of quartzite cobbles. You don’t need to import it thousands of kilometers, unlike Knife River Flint or obsidian. Not all quartzite is the same quality, but there are well documented sources of high quality quartzite and sandstone throughout the province, like the top of the Grizzly Ridge by Swan Hills or in the Oil Sands around Fort McMurray.
In fact, this point is made from a type of quartzite that is commonly known as ‘Salt-and-Pepper’ because of the small black specks in the largely white stone. This material has been found all over Northern Alberta, but it is most commonly reported around Fort McMurray. While no source has been officially documented, archaeologists who work in the Oil Sands region often report seeing raw cobbles and boulders of ‘Salt-and-Pepper’ quartzite in the creeks flowing into the Athabasca River. It is very likely then that this point was made from a cobble that came from the Fort McMurray region. Whether the person who made the point carried from Northeastern Alberta or if it made its way by trade, we don’t know. However, it does show us the vast ancient networks that connected the First Nations across Alberta.
So we know where the raw material for the point came from, what about how it was made? What can the shape and design tell us about the people who made it? One way to study this is to look at the flake scars, the ridges and concavities left when pieces of quartzite were struck from the point. Most of the time with finished projectile point, or those that have reached the end of their life as a usable tool, we will see that the edges will be very uniform and straight, with small flake scars along the blade where the tool was resharpened. However, this artifact is very rough, the edges are irregular and chipped and the blade has large long flake scars covering the surface. Based on these traits, it appears that this point was unfinished, and looking at where the break is, it was likely broken when they were trying to make the blade thinner. This point is what would be called a ‘Preform’, a roughly worked projectile point that has not been attached to a haft yet. Preforms can take a variety of shapes and forms, but they often resemble the final point style.
So now that we understand that we are looking at an unfinished point, it better explains why the shape of the artifact does not perfectly match other Alberta points. However, that doesn’t help us to determine if it is an Alberta, Hell Gap, or Taltheilei projectile point. The implications of assigning the point one of these time periods is significant, because it would move the occupation of the site from a period where Giant Bison and Ice Age mammals roamed Alberta during the Hell Gap Phase, to an environment more similar to what we see today during the Taltheilei Phase. Personally, I think that the point from GfQa-5 is more similar to projectile points and preforms that have been dated to the Hell Gap period. The shape of the shoulders, base, and the blade all seem to better match the style of these points than Alberta Points, and the points found at Taltheilei sites tend to be smaller and narrower. A cache of similar looking spear points were found near Eaglesham in northwestern Alberta, and the archaeologists who studied these points concluded that they were likely unfinished Hell Gap points. It seems likely then that the spear point I found would fall into this time period. However, this is still based on very general characteristics, and it could still easily fit within all three of these categories. Until we have more information, and we excavate more archaeological sites, we are often left with our best guess.
Last year, while conducting survey with Brittany in a remote region of northern Alberta, I noticed some unusual scarring on a large spruce tree. Upon closer examination I realized the tree had been struck by lightning.
Usually when lightning hits a tree, one of three things may happen:
If the tree is wet on the outside, the electrical discharge may travel down the outside of the bark to ground and have little effect on the tree itself.
If the tree is not wet, the discharge may travel down the tree on the inside of the bark, which will result in scarring. In my experience, this will usually be one or more scars that revolve around the trunk of the tree as the discharge travels downwards.
If the tree is not wet, but is full of moisture, the moisture may be super heated and instantly turn into gas that quickly expands and causes an explosion. This may blow the bark off the tree, blow the top off the tree, or in some circumstances completely destroy the tree.
The tree that Brittany and I stumbled across had a considerable amount of damage due to the lightning strike. Yet, even though the tree had substantial bark scarring and its top blown completely off, it did not die and seemed to be in pretty good shape.
As rare as finding a lightning tree may seem, trees are actually struck by lightning very frequently. The Government of Canada reports that there is an average of 2 million cloud to ground lightning strikes per year in Canada, igniting approximately 45% of all our forest fires. These fires account for nearly 80% of the total forests burned annually. Although I wasn’t aware of these statistics until recently, my time working as a Forest Fire Fighter made me very aware of the frequency, since many of the fires we were called to fight were started by lightning. Even during a torrential downpour, lightning may still strike a spruce tree, causing a small fire to start at the base where it is sheltered by the branches. Days or even weeks later, when the temperature rises and the vegetation dries out, the fire may grow substantially in size. Suppression of these fires cost Canadian taxpayers a substantial amount of money. The Government of Canada has a whole section of their website dedicated to severe weather.
Taking refuge under a tree during a thunderstorm is very unwise. It may seem like a good place to keep dry during a sudden downpour, but it is actually one of the most unsafe places you could be. Indoors is always the safest place to be. However, if you are caught without shelter in a thunderstorm, the best place to be is in a low lying area such as a ditch. You might not stay dry, but you will be safe from lightning. Just make sure you watch out for flooding!
If you do happen to stumble across a lightning tree like Brittany and I did, you may want to take a little token for yourself (as long as it doesn’t harm the tree if it is still alive). Many people believe that the wood from a lightning tree will bring you good luck. Others believe that the power passed from the lightning to the tree, can then be passed on to whoever possesses its wood. Even if you are all full up on power and luck, you could always just keep the wood as a souvenir and reminder of the raw and devastating power of nature.
Projectile points come in many shapes and sizes ranging from large paleolithic spear points to small protohistoric arrow heads to even smaller “toy arrow heads”. This artifact type is a stone that has been shaped using flint knapping techniques to create a sharp triangular and aerodynamic tip that is attached to a wooden shaft that can be propelled through the air by throwing by hand, atlatl, or bow, to hunt game. This is an important artifact type as over time the styles of points changed allowing us to use the style to estimate the time period a site was occupied. This particular point is a Besant style dart point, which dates to approximately 2,500 -1,350 BP.