Note: After June 1st, this attraction will be replace by Moraine Lake. Johnston Creek originates north of Castle Mountain in a glacial valley southwest of Badger Pass The creek flows through a gorge known as Johnston Canyon. As Johnston Creek approaches the Bow River, it flows through a large canyon formed by erosion over thousands of years. The creek has cut through the limestone rock to form sheer canyon walls, as well as waterfalls, tunnels, and pools.

Castle Mountain is a mountain located within Banff National Park in the Canadian Rockies, approximately halfway between Banff and Lake Louise. The mountain was named in 1858 by James Hector for its castle-like appearance

Note: Moraine Lake is available after June 1st. Moraine Lake is a world-famous glacially-fed lake nestled in the heart of Banff National Park, Alberta, Canada. Surrounded by the towering peaks of the Valley of the Ten Peaks

Lake Louise is a glacial lake within Banff National Park in Alberta, Canada. It is named after the Princess Louise Caroline Alberta, the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The turquoise colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km² and is drained through the 3 km long Louise Creek into the Bow River.

The village of Lake Louise is the highest mini town with an elevation of 1,661 m. Take some free time here to have your lunch, browse the stores and the visitor center surrounding the mini square. Regain some energy for the next 3 lakes of the tour.

Early explorers named the glacier Crowfoot because its three sections of ice looked like a crow’s foot on the mountain. While one of the three “toes” has now receded and disappeared, the glacier is no less spectacular. The Crowfoot Glacier sits above Bow Lake, providing stunning photo opportunities for those traveling the Icefields Parkway. The spectacular Crowfoot Glacier can be viewed from a lookout point on the world-famous Icefields Parkway about 34 km (21 mi) north of Lake Louise. Attached to the northeastern side of Crowfoot Mountain, overlooking Bow Lake, the glacier's runoff feeds into the Bow River, which flows from Banff National Park through the City of Calgary to the Alberta prairies.

Bow Lake is one of the many lakes that line the Icefields Parkway and a popular stop for visitors to Banff National Park in Alberta, Canada. It’s no secret that the Canadian Rockies are not short of spectacular vistas and lakes. Bow Lake is one of our top recommendations for a stop to stretch the legs on the Icefields Parkway. A short walk along the lakeshore trail is a family-friendly hike, or you can enjoy longer hikes around Bow Lake for a more complete day. Whatever you decide to do, make sure you don’t miss Bow Lake.

Peyto Lake is a glacier-fed lake in Banff National Park in the Canadian Rockies. The lake itself is near the Icefields Parkway. It was named for Bill Peyto, an early trail guide and trapper in the Banff area. The lake is formed in a valley of the Waputik Range, between Caldron Peak, Peyto Peak and Mount Jimmy Simpson, at an elevation of 1,860 m (6,100 ft). During the summer, significant amounts of glacial rock flour flow into the lake from a nearby glacier, and these suspended rock particles are what give the lake a unique bright, turquoise colour. Because of its bright colour, photos of the lake often appear in illustrated books,and the area around the lake is a popular sightseeing spot. The lake is best seen from Bow Summit, the highest point on the Icefields Parkway. The lake is fed by Peyto Creek, which drains water from Caldron Lake and Peyto Glacier (part of the Wapta Icefield). Peyto Lake is the origin of the Mistaya River, which heads northwest from the lake's outflow.

Emerald Lake is a freshwater lake located in Yoho National Park, British Columbia, Canada. Emerald Lake is enclosed by mountains of the President Range.

Natural Bridge is an impressive natural rock formation that spans the flow of the Kicking Horse River west of Field, where the slower-moving waters from the Field valley flats begin their descent through a canyon to be joined by the Amiskwi River. Sculpted by the erosive forces of rushing water over what had once been a waterfall, the Natural Bridge is a powerful reminder of how much influence water has in shaping the landscape. Softer rock found below the Natural Bridge's hard limestone band eroded more quickly, and fissures in the rock widened until the flow of water was diverted below the outcrop.