Overview and hiking guide to the old-growth forests of Stanley Park.
- Stanley Park Big Tree Tour: the major big tree areas connected via a three hour self-guided walk (in progress)
- Disturbance Ecology and History of the Stanley Park Forest
Stanley Park is the most visited and certainly the most cherished of Vancouver’s entire park system. However, most of the park’s 8 million annual visitors (Vancouver Park Board 2007) stick to the main attractions, and relatively few venture into the parks interior forests. Hidden inside the park’s canopy cloak are some of the most remarkable trees in Vancouver, let alone the entire province. There are groves to discover with monumental ancient cedars and towering Douglas-fir. In fact, record-sized specimens for some native tree species are concealed within this park, within ear shot of the busy downtown centre. In this guide, you will find directions to visit the largest trees of several species, and if you read on, you can acquaint yourself with stories surrounding the park’s interior forest ecology and natural history. I’ve created this page to help build readers sense of place, familiarity, and overall appreciation of Stanley Park. I do hope you enjoy.
2) Stanley Park Big Tree Tour: the major big tree areas connected via a three hour self-guided walk (in progress)
It is quite easy to visit the parks largest trees, including the thickest western red cedar at over 5m (16.5′) diameter and the tallest Douglas-fir at 65m (214.5′) tall. These productive conifer forests grow higher than mid-size skyscrapers in adjacent downtown. Perhaps, more significant than the parks coniferous giants are the parks deciduous trees. The park contains the largest recorded big leaf maple tree in BC (Acer macrophyllum), which is perhaps the largest Maple tree in Canada! (Unless this sugar maple (Acer saccharum) in Ontario is larger). At third beach, grows the largest recorded red alder in BC, though pruning may have reduced it to now being the second largest recorded red alder in BC.
Surprisingly, the parks incredible big trees are often overlooked due to the plethora of other recreational activities and the popular shoreline. Here, I am in the process of writing directions for exploring inside the park’s forested areas to see the largest specimens of a variety of native tree species found within the park. One of my goal’s is to update measurements of the parks largest trees, which have not been re-measured since originally measured in 1987 by Randy Stoltmann (1987).
Although it is believed that most of the tallest Douglas-firs in the park were logged by the 1930’s (Stoltmann 1987) the old-growth forests are still a vital legacy of Vancouver’s natural history. Due to the park’s high traffic and the obvious heritage value, please tread respectfully and, if you are in a group, considering keeping some distance from the most ancient trees to minimize trampling of their roots.
2.1) Easy to access large Douglas-fir near the Stanley Park Bus Loop
A couple fantastic Douglas-fir specimens are easy finds, just a few minutes from the bus loop. The southern most of the two is an astounding specimen, which showcases in plain site the straight growth of Douglas-fir. This giant provides a mysterious insight into just how tall can a Douglas-fir grow? In fact, its possible that this is the tree that is sometimes rumoured to have been above 90m in height near the park’s entrance. This tree is now broken off at around 55.5m, at which point it is still very thick and straight. A live branch is its highest point. The tree 50m to the north of it is less impressive as a specimen tree, but is still 51.1 m tall with a 1.9m dbh trunk. These tree may grow taller yet, but how could we ever know how tall they once grew…. ?
Well… lets speculate its former height! So, because this tree is well centred at the historical entrance of Stanley park it makes a clear appearance in numerous historical photos. I’m quite confident that our tree is seen below after having inspected from numerous angles (including Google Earth) of how the tree lines up with the entrance, the rowing club building, and the Stanley Park Pavillion. In 1921, it appeared to have had a mostly live and intact top, see below.
However, by 1936, at the time when the causeway was built, the top portion of its crown was sheared off (I would guess it was cut off for safety reasons). See below.
Now let’s line a couple of those shots up, make a few assumptions, and get a preliminary rough estimate of the tree’s historical height…
I’ve made several assumptions here: 1) that the trees in these photos are the same, 2) that I’ve lined up the trees properly based on conspicuous branching features, and 3) that I’ve accurately estimated the height of the base of the tree. I feel pretty good about assumptions 1 and 2, but not great about 3. Anyway, for now, if the tree as seen in 1936 is the same height as it is today (55.5 m), than the tree was a true giant at around 77.7m in height back in 1921 (and other photos show that it was still intact up to 1928). What I need to do now is to get additional modern photos to check if the 1931 height matches today’s height. Why does this matter? Well, I’ve heard that the tallest tree in the park once grew at the entrance, which simply must have been this tree in the historical photos unless it was cut down prior to 1921. Here is an opportunity to investigate the tree’s height, and potentially either support or refute the claim that this historic tree was over 90m in height.
2.2) The Tall Tree Grove
The Tall Tree Grove is a collection of large diameter trees once recorded to be the tallest in the park by Stoltmann (1987). The second tallest tree in this grove when measured in 1987 was a 72.5m dead tree known as the ‘Eagle Tree.’ This tree is frequently perched on by bald eagles, which carefully select their favourite perch trees. By my measure in 2016, the Eagle tree has lost ~9m of height and is now 63.5m tall with a dbh of 2.1m. A piece of broken crown, several meters in length, lay at its base, probably since at least ten years ago. There are also piles of bark that provide a warning that this is not a safe place to linger due to overhead debris hazards. The Eagle Tree is best enjoyed from Pipeline road, which gives a clear view. Directly beside Pipeline Road is a healthy Douglas-fir about 56 m in height. In 1987, another tree immediately uphill to the north had a dead top at 76.5m in height. This dead tree was nearly the tallest in the park, but by 2016, the tree has collapsed and is no longer visible —I have not yet searched for its remains. These dramatic losses of height in the grove appear to be due to wind, which has battered and thinned the canopy. In 2016, I observed a very large hemlock and red-cedar recently downed at the centre of the grove. These old trees together with the open canopy caused by wind battering has bestowed the grove with more character than nearly any other grove around Vancouver, the wind being a natural shaping agent, which I discuss in section 3 of this guide.
There are still several very large, easy to view Douglas-fir within the tall tree grove, including several of the widest-diameter Douglas-fir in the park. Find the widest Douglas-fir in the tall tree grove by heading northwest and uphill along ‘Tunnel’ path watching for the big trees off to the right side of the trail. The first tree you see (the eastern most large tree in the tall tree grove), is 2.2m dbh and 52.5m tall. It is somewhat difficult to access due to large fallen logs obstructing the way. Also, as of 2016 the tall tree grove is becoming formidably entangled by invasive (and very prickly) Himalayan blackberry. I suggest continuing slightly further on tunnel trail and to the right you cannot miss a very large diameter Douglas-fir tree only about 15 m off from the path. This tree can be easily visited and I encourage you to because it’s a giant at 2.4m dbh —one of the thickest Douglas-fir in the park —and is a beautiful specimen to observe the remarkably thick and furrowed bark of veteran Douglas-fir trees. Beside this are a very tall hemlock and two additional large Douglas-firs to your left. One of the Douglas-fir to your left has a dead and broken top measuring at ~55m. Head a little bit further down Tunnel until you’re almost at Pipeline Road and note the very large Douglas-fir stump on the left that is cut about 2.5 m above ground. This stump is nearly as thick as those remaining even without its bark. In fact, there are very large Douglas-fir stumps throughout the Tall Tree Grove and on Tunnel Trail heading east towards Lumberman’s Arch.
More big tree areas coming soon…
3) Disturbance Ecology and History of the Stanley Park forest
All forests are faced with various types of disturbance —there are fires that raze, insects that defoliate, and windstorms that topple trees— which shape forests through time in various ways. Disturbances come in varying intensities and leave their signatures in the form of legacies such as fallen logs and dead rotting stumps. These legacies provide us with clues for investigating a forest’s history. Old-growth forests, such as those found within Stanley Park have long and dynamic histories to share.
In the humid coastal margins of Vancouver we find a type of forest classified as coastal temperate rainforest. These forests are dominated by long-lived coniferous tree species. Forest fires are extremely rare in this forest type and disturbances are usually low in severity windstorms that uproot trees and knock out small clearings in the forest canopy. In an old-growth forest you’ll notice that the overhead canopy is quite open with many gaps that allow sunlight to enter the forest. Understory plants grow more vigorously in the enhanced light under canopy gaps and conifer seedlings are able to establish, to one day grow tall and establish a spot in the canopy high above. The wind sometimes breaks trees clean in half leaving tall sections of trees that remain dead but still standing, which begin to decay and provide foraging habitat for pilleated woodpeckers. When wind knocks trees to the ground sometimes the logs stack on top of each other creating a matrix of logs crisscrossing the forest floor. The influence of windstorms on forest development is written into the unique identity of old-growth forests, and there are few places where you can see this as clearly as in Stanley Park.
pdf of map highlighting some of the major changes from year to year: Stanley Park aerial photograph sequence 1946-2008
Figure. Gallery of aerial photos 1946 – 2015 to highlight changes in the parks forests caused by wind. Final slide summarizes the extent of damage caused by the 2006 windstorm and Hurricane Freda in 1962. Images 1946-2008 are extracted with permission from the MSc thesis of Mike Buffo (2010), and originally come from UBC Geographic Information Centre library. 2015 photo comes from Google Earth.
Occasionally, destructive windstorms occur in our local coastal temperate forests. In Stanley Park, damaging windstorms in 1934, 1962 and most recently in 2006 arrived and knocked over huge swaths of forest. Wind has been a major driving influence on the park’s forest ecology, but the 2006 windstorm was more severe than any other to hit the park in the past 100 years. The 2006 windstorm ravaged 80ha of forest, causing severe damage to a full 30ha of forest. Severe damage is defined here as >60% of the canopy being affected —rarely does wind knock over such stands entirely.
Both Hurricane Freda in 1962 and the 2006 windstorm damaged many large trees and left legacies in the form of young recovering stands, which are distinct in species composition and structure from the old-growth forest. Relative to the old-growth, the stands recovering from Freda are either now dominated by deciduous trees (i.e. to the south of Beaver Lake) or are young conifer stands. Many trees of similar size and age characterize the structure of these young stands. As they grow upwards they strongly compete for light excluding light transmission for understory plants. Meanwhile, the stands recovering from the 2006 windstorm have small conifer saplings (many of which were planted) below the leftover standing trees not blown over by the wind. These areas provide an obvious impression that something powerful swept through.
Coming soon… the legacies of logging and forest management in Stanley Park
Bakewell, David R. “Forest maintenance program for Stanley Park.”Commissioned by Vancouver Board of Parks and Recreation (1980).
Buffo, Mike A. Meeting management goals in an urban forest: vegetation dynamics and prescriptions in Stanley Park.” Electronic Theses and Dissertations (ETDs) 2008+ (2010).
Vancouver Park Board. Stanley Park Restoration Plan. Vancouver Park Boards and Recreation, Vancouver (2007)