14. Dry Haven–Goldeye Lake Connector

Map C (p. 62)

Duration two hours
Distance 4.8 km
Level of Difficulty easy stroll
Maximum Elevation 1370 m
Elevation Gain 10 m
Map 83 C/8 Nordegg

Access: Park your vehicle at the Dry Haven Recreation Area, located 11 km south Nordegg or 88 km north of the Banff National Park boundary.

0.0 kmtrailhead

0.3 kmturnoff for the Centre for Outdoor Education

0.4 kmjunction

0.7 kmcutline

1.5 kmcutline

1.6 kmjunction

1.8 kmjunction

2.0 kmBlack Canyon Creek bridge

2.0 kmjunction

2.4 kmGoldeye Lake and Recreation Area parking lot

4.8 kmtrailhead

For campers at the Dry Haven Recreation Area, this is an easy 2.4 km stroll to Goldeye Lake.

From the Dry Haven campground, cross Highway 11, turn right and walk 300 m to where you will come to the turnoff for the Centre for Outdoor Education (COE). Walk down the gravel road 100 m. Just before the road takes a 90-degree bend to the left and dips down a slope to go to the COE, there is a track straight ahead that you need to take. A cutline and trail will come into view on the right. Follow the cutline until it intersects with another cutline. Turn left and find a trail on the right after 100 m. Bear right onto this trail and follow it to a junction beside Goldeye Lake. Bear right. At a junction just past Black Canyon Creek, bear left to reach Goldeye Lake and its promise of a cooling swim.

Historical Footnotes: Goldeye Lake

Goldeye, a popular, silver-coloured sport fish, was stocked in this lake in the 1940s, thereby lending its name to these waters. Today, goldeye are not found in this lake; indeed, they are only found in the North Saskatchewan River downstream from Rocky Mountain House. Goldeye Lake is stocked, however, with rainbow trout, making it a popular fishing spot. Fishermen using boats are restricted to electric motors. Another name for Goldeye Lake, still in some local use, is Pine Tree Lake.

Coring a lake in northern Alberta to recover sediment for pollen analysis. Here a three-metre-long collecting tube has been lowered to the lake floor through a hole cut in the ice surface. The tube is being driven into the sediments to collect a continuous sample. Then the tube will be pulled to the surface, capped and returned to the laboratory so the contained sediments can be analyzed. Courtesy of the Royal Alberta Museum

During the 1980s and ’90s, researchers from the University of Alberta conducted palynological research at a number of sites along the eastern slopes of the Rocky Mountains, including Gold-eye Lake. They drew core samples from the bottom of the lake to extract the pollen trapped in the mud. By studying the ancient pollen, the researchers learned what plants grew in the area, and, therefore, what the climate and landscape were like thousands of years ago.

At the height of the last ice age, around 18,000 years ago, the eastern slopes would have mostly been covered by ice. As the climate began to warm, ice melted and bare ground was exposed. The first vegetation at the end of the last ice age around Gold-eye Lake was tundra-like, with some shrubs but no trees. The most common pollens were from willow, sage, grass and sedge plants. As the climate began to moderate, more trees appeared in the area, including aspen, spruce, birch and pine, and the land became more forested. First, birch and poplar formed an open woodland; then conifers became more prevalent. By about 10,000 years ago, the forest vegetation around Goldeye Lake would have looked quite similar to that seen here today.