Baker Lake, the geographical center of Canada

Baker Lake is a native village located near the geographical centre of Canada:

Baker Lake sits inland, in a tundra forest region at the mouth of the Thelon River into the Baker lake.

Caribou crossing Thelon river at Baker lake

Other major rivers - the Kazan and the Dubawnt - flow into Baker lake. The lake is also connected to Hudson Bay by way of Chesterfield Inlet.


The local Inuit name this village as Qamani’tuuq, meaning, “where the river widens”.

Coordinates: 64'18' N, 96'04' W
(sub-artic).

Baker Lake, or Qamani'tuaq, pop. 1800.

The hamlet was founded in 1961, and has been growing due to local mining.
It has a health center, small hotels, swimming pool, library, primary and secondary school, youth centre and three small churches.

The main front, looking at the lake.

The hamlet in winter

New Jonah Amitnaaq Secondary school.

Inns North, a odd-looking arctic hotel

The local Northern Store

A Church in the snow

Baker Lake is an intriguing example of a modern day arctic community, for the amazing growth of its artistic community. With Cape Dorset and Pangnirtung, Baker Lake is well known for its inuit arts and craft activities.

The Jessie Oonark Centre

Distinguished artists and studios promoting arts and crafts, such as the Jessie Oonark Centre, and well-established independent art galleries, are famous for the quality of their art.

The old Hudson Bay Company store

The Vera Akumalik Visitor Centre is located in the original historic Hudson's Bay Company Post near the waterfront:


The centre is a replica of the old store. Staff will help arrange local tours, and will make suggestions on local walks to appreciate the beauty of the rivers and the tundra.


The Rivers

The Baker lake drains through Chesterfield Inlet into Hudson Bay.

North Channel of Chesterfield Inlet

Musk oxen herd at Chesterfield Inlet

The Kazan River flows north for 732 km before discharging into the southeastern corner of Baker lake.

Beautiful Kazan Falls, where the water drops 25 m and rushes through a red sandstone gorge.

Kazan falls

The Thelon River is one the great rivers of the North.


It flows eastwards 904 km to discharge into Baker Lake and Chesterfield Inlet. The river's middle and lower reaches have been designated as a Heritage River.

For the Inuit of Baker Lake, these rivers are a vital source of caribou, fish and spiritual renewal. Not only did the Inuit People live near and around these rivers, but they provided the means and the route to the North for many of the Europeans that traveled and traded in that area.

Antarctic summer colours

Summer in Antarctica lasts 6 months, from October to March. During the central 4 months, 24 hours of complete daylight allow a summer temperature maximum around 2°C.

What about flora? Everybody knows about antarctic fauna - seals, penguins, birds - but are there some flowers ? Like the beautiful arctic flowers ?

Well, life is really hard for plants there. There are several mosses, fungi and lichens , but just two kinds of native flowering plants manage to grow:

- a fine-leaved, perennial grass, the Antarctic hair grass (Deschampsia antarctica), one of only two flowering plant species living below latitudes of 60 degrees:



- and Antarctic pearlwort (Colobanthus quitensis), that has white flowers and grows about 5 cm tall, with a cushion-like growth habit that gives it a moss-like appearance:




They are present mainly in the 1% of the region that is ice and snow free, along the warmer parts of the Antarctica Peninsula and in the South Orkney Islands and the South Shetland Islands.
Small clusters of the Antarctic hair grass can be seen among rocks and in moss-filled cracks in the bedrock.
Moss - on the better drained, stony slopes of the Antarctic Peninsula, mosses build up to a deep peat - as much as six and one half feet deep and 5000 years old !

Lichens - more than 350 species. They have proliferated in Antarctica because there is little competition from mosses or flowering plants.

Piteraq in Kuummiut - Greenland at its best and worst

From Carl Skou's Kuummiut blog, I got this amazingly beautiful video:
(listen to the atmospheric music)



A violent Piteraq storm strikes Kuummiut village in March 2011. The Piteraq is a katabatic wind. Intensely cold heavy air drains off the Greenland ice cap. The cold descending air is channelled through the valleys and can blow at 40-80 metres per second. The Piteraq is characterised by deep blue skies, intense sunlight, clear dry air and much blowing snow which can obscure visibility. Most people stay indoors during a Piteraq. This Piteraq followed a period of overcast weather and heavy snowfall. The Piteraq strips the snow from the land and breaks up the fjord pack ice.

Saksun, the spirit of the Faröe Islands

The Faröe Islands are one of the most credible candidates to Ultima Thule !

Situated half way between Scotland and Iceland in the Northeast Atlantic, the Faröe Islands (Føroyar) are an archipelago of 18 fantastic mountainous islands, and a population of just over 47000.

Sea, green hillsides, sharp cliffs and mountains, strangely shaped islands, turf-roof houses...

and a gorgeous capital, Tórshavn:

Saksun, Streymoy island

Location: 62°14′56″ N, 7°10′33″ W

Saksun is a village near the north-west coast of the Faroese island of Streymoy.

Saksun was once an inlet surrounded by high mountains. The inlet formed a deep and good natural harbour. However a storm blocked the inlet with sand.

This made the old harbour become a unaccesible seawater lagoon.

Saksun is now a picturesque village in the bottom of the lagoon.

The Dúvugarður Museum occupies a seventeenth century farm house

The old turf-roofed farm house is a well-preserved example of a Faroese farmhouse of the 17-19th centuries.

On display here are many old domestic utensils and household objects and furniture, which displayed in their original context help to give a lively impression of traditional life in the Faröes.

The beautiful church in Saksun was built in 1858 :

Repairing the turf roof :