| Point Pelee National Park | |
|---|---|
IUCN category II (national park)
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Boardwalk in April
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Location of Point Pelee National Park in Canada
| |
| Location | Ontario, Canada |
| Nearest city | Leamington, Ontario |
| Coordinates | 41°57′51″N 82°31′4″WCoordinates: 41°57′51″N 82°31′4″W |
| Area | 15 km2 (5.8 sq mi) |
| Established | 1918 |
| Governing body | Parks Canada |
| Official name | Point Pelee |
| Designated | 27 May 1987 |
| Reference no. | 368 |
History
Aboriginal people lived on Point Pelee for a long time before European colonization, dating back to at least 6,000 years. The largest archaeological site found at Point Pelee is thought to have been occupied between AD 700 and 900.
The name was given to the area by Fathers Dollier and Galinee when they passed through the area in 1670.
In the late 1700s, British naval reserves logged the area's white pine for shipbuilding.
In 1790, Deputy Indian Agent Alexander McKee negotiated a treaty with
Aboriginal communities that ceded a large tract of land, which included
Point Pelee, to the Crown. The Caldwell First Nation
Chippewa people, who inhabited Point Pelee, were not signatories of
that treaty. However, the Crown did not realize this, and their land was
ceded nonetheless. Subsequently, they were forced off their land, and
Point Pelee remains unceded aboriginal land. This has been publicly
acknowledged by the Department of Indian and Northern Affairs Canada.
Prior to the creation of the park, the Great Lakes Ornithological
Club was established to study bird migration. One of the members, Percy A. Taverner, and Canada's first Dominion Ornithologist, recommended Point Pelee be made a national park in 1915. Jack Miner had also pushed for the creation of the park by that time. Point Pelee was made a national park in 1918 at the urging of birdwatchers
and hunters. Commercial fishing continued in the park until 1969. Point
Pelee was the only Canadian national park to allow hunting until duck
hunting was ended in 1989. This site was named "Pointe-Pelée" (meaning
"bald point" by French explorers because the eastern side was rocky and had no trees).
Point Pelee was designated a dark-sky preserve in 2006, having become the first Canadian national park to be designated as such. In March 2006, high winds caused waves that washed away the sand point and all that remained was a platform.
In October 2007 the level of Lake Erie dropped enough to reveal the
point again extending at least a kilometre out into the water and at
least 7 metres (23 ft) wide with a winding curve shape to it. Since that time the sandy tip continues to shift, grow longer or shorter, or even detach temporarily, from year to year.
Geography
Pelee Island location
Located in the western parts of the St. Lawrence Lowlands, the park is a sandspit formation that extends 15 kilometres (9.3 mi) into Lake Erie and is up to 70 metres (230 ft) thick. With an area of only 1,564 hectares (3,860 acres), it is Canada's smallest national park. Most of the park (about 1,113 hectares (2,750 acres) or 70% of the park consists of marsh, dominated by cattails and ponds although forested areas make up a significant portion of the park, covering about 21% of the park. This sandspit is dominated by till plains which was formed during the last ice age during the advance and retreat of the Wisconsonian ice
on a submerged limestone ridge. As the glacier melted and retreated
northward, the Lake Erie basin began to fill with water. The movement of
sediments altered the coastline, resulting in the present day shape of
Point Pelee. Subsequently, over the centuries, a thin but rich soil has formed. Mineral soils in the park were mapped as well to rapidly drained Eastport sand, which has insignificant profile development. The marshes began to form about 3,200 years ago, based on carbon dating. This was also the same time when the sands began to deposit, forming the present day barriers.
The marsh has a closed drainage system owing to the separation of it by
two barriers along the east and west side, which usually prevents the
free exchange of water. However, when lake levels are higher, the marsh water levels fluctuate with the lake's water levels. The distinctive triangular shape at the southern tip of Point Pelee is caused by the convergence of these two barriers.
Middle Island, which is located south of the Point Pelee peninsula has
an area of approximately 18.5 hectares (46 acres) and is the southernmost point in Canada. Virtually all of Middle Island is forested.
Flora and fauna
Barn swallows (Hirundo rustica) at Point Peele National Park in May 2010
Owing to its southernly location and the moderating effects of Lake
Erie, the climate in the park is slightly warmer than the rest of Canada and many Carolinian faunal species, which are rare in Canada are located here. Examples include the fox snake and the five-lined skink.
Because of its location at the crossroads of 2 major migration flyways,
about 347- 360 different species of migratory birds have been recorded
in the park and more than 100 species stay there for breeding. This total includes 102 waterfowl and shorebird species. Dominic Couzen's Top 100 Birding Sites of the World lists Point Pelee as #66. Coyotes and martens are also present within this park.
Many Carolinian floral species that are rare in Canada occur within the
park boundaries. The park contains more than 750 native plant species, of these 8 species are considered to be rare, endangered or threatened in Canada. Nearby Middle Island is designated provincially as an Area of Natural and Scientific Interest (ANSI) due to its unique and rare assemblages of plants and animals.
Middle island is home to plants and animals that are characteristic of
the Carolinian ecozone of which nine species are at risk.
The diversity of vegetation in the marsh is the highest along the edge
of the marsh ponds and in the transitional zones between the terrestrial
environments and the marsh. Four different vegetation communities dominate in the marsh.
Climate
Point Pelee has a humid continental climate (Dfa under the Köppen climate classification) with warm, humid summers, and cold winters that is modified by the surrounding waters of Lake Erie. It lies in a zone that is characterized by variable weather due to conflict between polar and tropical air masses.
Its position in Lake Erie modifies its climate, resulting in warmer
winter and fall temperatures compared to inland regions, as the lake
cools more slowly than the surrounding land though during the spring,
temperatures remain cooler than inland areas due to the land warming
faster than the lake.
Winters are cold with a January average temperature of −3.9 °C
(25.0 °F). Owing to its position in Lake Erie, winter temperatures are
warmer than inland locations at a similar latitude due to the release of
the heat stored by the lake.
As a result, temperatures below −20 °C (−4.0 °F) are rare, with only
1.9 days where the temperature reaches or falls below −20 °C (−4.0 °F).
The maximum temperature usually stays below freezing on most days
although mild spells of weather can occur time to time. The park
receives 98.9 centimetres (38.9 in) of snowfall per year and there are
30.6 days with measurable snow. The park is not located in the snowbelt region, and snow cover is intermittent through the winter.
Summers are warm and humid with the warmest month, July, averaging 22.4 °C (72.3 °F), which is among the highest in Ontario. The surrounding lake moderates summertime temperatures, cooling the flow of warm air masses originating from the Gulf of Mexico and as a result, temperatures above 30 °C (86.0 °F) are rare, with only 4–8 days per year in the park.
| Climate data for Point Pelee National Park | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Record high °C (°F) | 13.0 (55.4) |
14.5 (58.1) |
22.5 (72.5) |
28.5 (83.3) |
31.5 (88.7) |
33.5 (92.3) |
34.0 (93.2) |
34.5 (94.1) |
31.0 (87.8) |
25.5 (77.9) |
20.6 (69.1) |
18.5 (65.3) |
34.5 (94.1) |
| Average high °C (°F) | −0.8 (30.6) |
0.3 (32.5) |
5.0 (41.0) |
11.6 (52.9) |
18.1 (64.6) |
23.6 (74.5) |
26.8 (80.2) |
25.7 (78.3) |
21.6 (70.9) |
15.0 (59.0) |
8.3 (46.9) |
1.9 (35.4) |
13.1 (55.6) |
| Daily mean °C (°F) | −3.9 (25.0) |
−3 (27) |
1.4 (34.5) |
7.4 (45.3) |
13.7 (56.7) |
19.4 (66.9) |
22.4 (72.3) |
21.5 (70.7) |
17.6 (63.7) |
11.4 (52.5) |
5.5 (41.9) |
−0.7 (30.7) |
9.4 (48.9) |
| Average low °C (°F) | −6.9 (19.6) |
−6.2 (20.8) |
−2.2 (28.0) |
3.1 (37.6) |
9.3 (48.7) |
15.1 (59.2) |
18.0 (64.4) |
17.2 (63.0) |
13.6 (56.5) |
7.8 (46.0) |
2.6 (36.7) |
−3.3 (26.1) |
5.7 (42.3) |
| Record low °C (°F) | −27.0 (−16.6) |
−24.0 (−11.2) |
−18.0 (−0.4) |
−9.8 (14.4) |
−3.2 (26.2) |
3.0 (37.4) |
7.0 (44.6) |
4.0 (39.2) |
−1.7 (28.9) |
−5.5 (22.1) |
−9.4 (15.1) |
−23.0 (−9.4) |
−27.0 (−16.6) |
| Average precipitation mm (inches) | 57.2 (2.25) |
58.7 (2.31) |
69.9 (2.75) |
75.6 (2.98) |
76.9 (3.03) |
79.8 (3.14) |
83.6 (3.29) |
85.9 (3.38) |
92.7 (3.65) |
69.6 (2.74) |
94.8 (3.73) |
77.4 (3.05) |
922.1 (36.30) |
| Average rainfall mm (inches) | 27.9 (1.10) |
31.3 (1.23) |
51.7 (2.04) |
71.7 (2.82) |
76.9 (3.03) |
79.8 (3.14) |
83.6 (3.29) |
85.9 (3.38) |
92.7 (3.65) |
69.6 (2.74) |
90.9 (3.58) |
56.8 (2.24) |
818.8 (32.24) |
| Average snowfall cm (inches) | 30.5 (12.0) |
27.3 (10.7) |
18.4 (7.2) |
3.8 (1.5) |
0.0 (0.0) |
0.0 (0.0) |
0.0 (0.0) |
0.0 (0.0) |
0.0 (0.0) |
0.06 (0.02) |
3.6 (1.4) |
20.0 (7.9) |
103.8 (40.9) |
| Average precipitation days (≥ 0.2 mm) | 13.4 | 11.4 | 12.8 | 14.7 | 13.3 | 11.7 | 10.9 | 10.1 | 11.7 | 13.5 | 15.3 | 15.4 | 154.4 |
| Average rainy days (≥ 0.2 mm) | 4.7 | 4.9 | 9.0 | 14.0 | 13.3 | 11.7 | 10.9 | 10.1 | 11.7 | 13.5 | 14.2 | 8.9 | 127.1 |
| Average snowy days (≥ 0.2 cm) | 9.2 | 7.1 | 4.7 | 1.3 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.15 | 1.7 | 7.5 | 31.6 |
| Source: Environment Canada | |||||||||||||
Human impact
Development
From
a regional perspective, the park is isolated from other natural areas
because in Essex County, less than 6% of the native forest cover and 3%
of the wetlands remain intact. Much of the area (97% of it) has been altered and mostly converted for agriculture, industry or urban development. It is also located close to major urban areas.
Bird-watching
It
forms the southernmost point in mainland Canada (its latitude is the
same as that of the northernmost counties of California) and is part of a
bird and butterfly migration corridor over Lake Erie via Point Pelee
and the Lake Erie islands. Over 360 bird species have been recorded in
the park. The peak time for bird migration is spring, especially May, when tired migrants make first landfall after their journey north across the lake.
Many birdwatchers from North America and abroad visit the park in May, often staying in the nearby town of Leamington.
One attraction, apart from the sheer numbers and variety of bird
passing through on migration, is the opportunity to see more northerly
breeding species such as blackpoll warbler before they move on.
Occurrences
March 2017 marsh fire
On
29 March 2017, Point Pelee's marsh land was involved in a fire causing
over 125 hectares (310 acres) of marsh habitat to be destroyed. The fire
lasted 15 hours and was naturally extinguished due to rainfall the
following day.
Commemoration
Point
Pelee National Park was featured on a high-value ($5) postage stamp,
issued in 1983, as part of a series honoring national parks. The park
appeared on a stamp that was issued on 15 January 2018, with a $1.20
face value. The issue coincides with the park's centennial year, and is
part of a nine-stamp set featuring scenic views across the country.
Images
Point Pelee tip looking south in 2007
Point Pelee looking South in April 2008
Point Pelee tip looking north in 2007
Boardwalk across a marsh in the park
Boardwalk in August
Point Pelee looking Southwest, January 2015
One of Point Pelee's shuttles
