12 places in 4 countries · updated 13 October 2026
In short: By our ranking, the most beautiful lakes in North America are Lake Louise (Canada), Lake Tahoe (United States) and Lake Atitlán (Guatemala). The list covers 12 lakes in 4 countries. Canada has the most, with 7. Last updated 13 October 2026.
North America's most famous lakes are gifts of the ice. Glaciers carved the valleys of the Canadian Rockies and still feed them with rock flour, fine particles that hang in the water and scatter light into shades of turquoise and jade. Elsewhere the continent's lakes come from fire and chemistry: water gathered in volcanic calderas, salt lakes trapped in desert basins, and mineral pools that dry into strange patterns each summer.
Canada's Rockies lead the list. Lake Louise sits beneath the Victoria Glacier, Moraine Lake mirrors the Valley of the Ten Peaks, and Peyto Lake, seen from above, has the outline of a wolf's head. Maligne Lake in Jasper holds the small wooded Spirit Island, while Emerald Lake in Yoho and Lake O'Hara are ringed by forest and steep peaks. In British Columbia, Spotted Lake dries in summer into dozens of mineral pools of different colours and is sacred to the Okanagan people.
The United States adds contrasts. Lake Tahoe, high in the Sierra Nevada, is famous for its deep, clear water, while Mono Lake, a salt lake east of Yosemite, is studded with towers of tufa. Colorado's Hanging Lake sits on a ledge of travertine fed by waterfalls. In Guatemala, Lake Atitlán fills a volcanic caldera surrounded by three volcanoes, and Trinidad's Pitch Lake is the largest natural deposit of asphalt in the world.
In this list
| # | Place | Type | Country | UNESCO |
|---|---|---|---|---|
| 1 | Lake Louise | Lake | Canada | |
| 2 | Lake Tahoe | Lake | United States | |
| 3 | Lake Atitlán | Lake | Guatemala | |
| 4 | Peyto Lake | Lake | Canada | |
| 5 | Mono Lake | Lake | United States | |
| 6 | Moraine Lake | Lake | Canada | |
| 7 | Pitch Lake | Lake | Trinidad and Tobago | |
| 8 | Maligne Lake | Lake | Canada | |
| 9 | Emerald Lake (Yoho) | Lake | Canada | |
| 10 | Spotted Lake | Lake | Canada | |
| 11 | Lake O'Hara | Lake | Canada | |
| 12 | Hanging Lake | Lake | United States |
Canada51.412° N 116.228° W

For the Stoney Nakoda people the lake was Ho-run-num-nay, the lake of little fishes. The first non-Indigenous visitor was Tom Wilson, a packer and outfitter who was brought here in 1882 by the Stoney guide Edwin Hunter and called it Emerald Lake. The name did not last: it was renamed for Princess Louise Caroline Alberta, a daughter of Queen Victoria and wife of the Governor General of Canada.
Did you know? In 1896 the climber Philip Stanley Abbot fell to his death on Mount Lefroy above the lake, often described as North America's first recorded mountaineering fatality.
United States · 24.8 km from Carson City39.083° N 120.033° W

What people come for is the water itself, famous for its transparency and for the ring of mountains reflected in it on every side. Clarity, though, is also its great worry. Long-term measurements by scientists at UC Davis showed visibility falling for decades as nutrients and fine sediment washed in, and the lake has become a test case for how development around a mountain lake is policed. It never freezes, and its deep water mixes only occasionally.
Did you know? The lake holds about 150 cubic kilometres of water, enough to flood all of California roughly 3 centimetres deep.
Guatemala · 8.3 km from Sololá14.700° N 91.200° W

What turns a deep lake into one of the famous views of the Americas is the skyline. Three volcanoes rise from its shores — San Pedro, the oldest, long inactive; Tolimán; and Atitlán, the youngest, formed within the last ten thousand years and last in eruption in 1853. Their cones stand one behind another above the water, and the light on them changes by the hour. Aldous Huxley compared it to Lake Como with "several immense volcanoes" added. Afternoons often bring the Xocomil, a wind whose Kaqchikel name is usually translated as "the wind that carried away sin"; it can whip the calm morning surface into steep waves.
Did you know? The eruption takes its name from the chocoyo, a parakeet that likes to nest in the soft layer of ash it left behind.
Canada51.725° N 116.522° W

The colour comes from the Peyto Glacier, an outlet of the Wapta Icefield, which sends meltwater down Peyto Creek and into the lake each summer. The water carries fine rock flour ground by the ice, and the suspended particles scatter sunlight into the vivid, opaque blue-green that has made the lake a fixture of calendars and books about the Rockies. The intensity varies with the season and the glacier's melt, at its strongest in the height of summer. Around the valley stand Caldron Peak, Peyto Peak and Mount Jimmy Simpson, and from the lake's northern end the Mistaya River begins its run down the valley.
Did you know? The glacier's first known record is an 1896 photograph by the explorer Walter Wilcox, and systematic research on it began in 1965.
United States38.017° N 119.009° W

The tufa towers people come to photograph are essentially frozen plumbing. Underwater springs rich in calcium bubble up through the lake's carbonate-heavy water, and where the two meet, calcium carbonate precipitates and slowly builds columns over centuries. The ones you see standing in open air today aren't new — they only became visible once the lake dropped low enough to expose formations that grew fully submerged. In a very literal sense, the tufa towers are a measuring stick for how much water has been taken from the lake.
Did you know? Each summer the lake teems with an estimated 4 to 6 trillion brine shrimp of Artemia monica, a species found nowhere else.
Canada51.322° N 116.186° W

The explorer Walter Wilcox reached the shore in 1899 and named the lake after the great heap of boulders at its northern end, which he took for a glacial moraine damming the water. Geologists now agree that the pile is the debris of rockfalls from the Tower of Babel, the 500-metre quartzite tower just to the south, which Wilcox also named for its outline. It is this rockpile that gives the classic view: a short trail of about 300 metres climbs its top, and from there the whole lake, the forest and the peaks line up in the picture that appeared on the back of the Canadian twenty-dollar note in its 1969 and 1979 issues.
Did you know? All but three of the ten summits were later renamed after people; Wenkchemna Peak still carries the Stoney word for ten.
Trinidad and Tobago · 19.2 km from San Fernando10.232° N 61.628° W

Its origin lies deep underground. The lake is thought to sit where two faults intersect, linked to the subduction zone under the Caribbean Plate, allowing oil from a deep reservoir to be pushed to the surface. Under the tropical sun the lighter components evaporate, leaving the heavy asphalt behind, mixed with clay. The asphalt is far from lifeless: researchers have found active communities of bacteria and archaea in it, including previously unknown species, and fungi able to live on asphaltenes alone; their activity releases bubbles of methane, carbon dioxide and hydrogen sulphide.
Did you know? In 2014 scientists reported that tiny water droplets of just one to three microlitres, trapped in the lake's oil, hold active microbial communities that digest the surrounding hydrocarbons.
Canada52.664° N 117.534° W

The celebrated view is of Spirit Island, a small tongue of land carrying a cluster of spruce, set against the mountains at the narrows partway down the lake. It is among the most photographed scenes in the Canadian Rockies, and it is reached only by water; seasonal boat tours run there from spring to autumn. In Stoney Nakoda it is called Githni-mi-Makoche, the healing island; it is sacred to the Stoney people, and visitors see it from a viewing area on the shore rather than setting foot on it.
Did you know? Henry McLeod, surveying routes for the Canadian Pacific Railway, glimpsed the lake from high in the mountains in 1875 but never went down to it.
Emerald Lake
Canada51.444° N 116.531° W

The lake lies at about 1,200 metres in a basin that catches weather: summers bring frequent showers, and winters heavy snow. It freezes from November until late April or early May, so its famous colour is a seasonal thing, deepening through the summer as glacial melt brings more rock flour. On still days the reflections of forest and mountain are almost perfect.
Did you know? Thanks to that banknote, Mount Burgess is still informally known as Ten Dollar Mountain.
Canada49.078° N 119.567° W

For the Syilx Okanagan people the lake is kłlilx'w, often written Kliluk, a sacred place of healing whose waters and muds have been used for centuries, each circle believed to hold its own healing properties. The lake passed into private hands in the colonial era; during the First World War its salts were dug out and shipped for use in ammunition manufacture, and for around forty years afterwards the land was owned by a local family. In 2001 the Okanagan Nation bought back 22 hectares around the lake, with most of the cost paid by the federal government, and it remains a protected cultural site under Syilx care.
Did you know? Besides magnesium, calcium and sodium sulfates, the water holds high levels of eight other minerals and small traces of silver and titanium.
Canada51.356° N 116.330° W

Within a few hours on foot from the shore lie Lake Oesa, a jewel-blue tarn in a rock amphitheatre, reached on a path that climbs beside a waterfall; the Opabin Plateau, a grassy shelf scattered with small lakes and larches; and Lake McArthur, known for an especially deep blue. More ambitious walkers can link high ledges into an alpine circuit far above the main lake. In late September the larches on the plateaus turn gold, and the contrast with the blue water is extraordinary.
Did you know? Robert O'Hara kept returning to the valley to explore its lakes, creeks and peaks after McArthur described it to him.
United States · 12.9 km from Glenwood Springs39.602° N 107.192° W

The lake owes its existence to geology at work right now. Dead Horse Creek runs through Mississippian limestone, dissolving carbonate as it goes; where the water slows and spreads, the carbonate is deposited again as travertine on rocks, logs and the lake's rim. Over time that crust built the delicate shoreline that holds the lake in place, and the same dissolved minerals give the water its unreal colour. The basin itself formed when a block of the valley floor, around six-tenths of a hectare, sheared off along a fault and dropped, leaving a hanging shelf above the canyon. In 2011 the site was designated a National Natural Landmark.
Did you know? The carbonate that builds the lake's travertine rim is dissolved out of the Leadville Limestone, a rock formation of the Mississippian period.
Places are chosen for how they look, not for how famous they are: each one has its own description and a photograph credited to its author. The order is a single world ranking that weighs the beauty of the place in curated photography together with how widely it is documented — the number of language editions of its encyclopedia article and how often that article is read in a year. The list is rebuilt as places are added, so the order and the counts on this page are always current.