Western Brook Pond

{{Short description|Fjord or lake in Newfoundland and Labrador, Canada}}

{{Infobox body of water

| name = Western Brook Pond

| image = Western Brook Pond.JPG

| caption =

| image_bathymetry =

| caption_bathymetry=

| location = Gros Morne National Park, Newfoundland, Newfoundland and Labrador

| coords = {{coord|49|46|08|N|57|49|14|W|region:CA-BC_type:waterbody_source:http://www4.rncan.gc.ca/search-place-names/unique/AAWUZ|name=Western Brook Pond|display=inline,title}}

| pushpin_map = Canada Newfoundland and Labrador

| pushpin_label_position =

| pushpin_map_alt =

| pushpin_map_caption = Location in Newfoundland and Labrador

| coor_pinpoint =

| coordinates_footnotes = {{cite cgndb|id= 59e5a809d05511d892e2080020a0f4c9|title= Western Brook Pond|accessdate= 2014-05-20}}

| type = Fjord

| inflow = Stag Brook

| outflow = Western Brook

| catchment = {{convert|171|km2|abbr=on}}

| basin_countries = Canada

| length = {{convert|16|km|abbr=on}}

| width =

| area = {{convert|23|km2|abbr=on}}

| depth = {{convert|72.5|m|abbr=on}}

| max-depth = {{convert|165|m|abbr=on}}

| volume =

| residence_time = 15.4 years

| shore = {{convert|42.5|km|abbr=on}}

| elevation =

| islands =

| cities =

| frozen =

|reference = {{cite web

| last =

| first =

| authorlink =

| title = Western Brook Pond

| work =

| publisher = World Lakes Database

| url = http://www.ilec.or.jp/database/nam/nam-31.html

| doi =

| accessdate =2008-03-05 }}

}}

Western Brook Pond is a Canadian fjord or lake located in Gros Morne National Park on the west coast of the island of Newfoundland. It is in the Long Range Mountains, the most northern section of the Appalachian Mountains.

File:NLW GrosMorne6 tango7174.jpg

File:NLW GrosMorne7 tango7174.jpg

File:NLW GrosMorne8 tango7174.jpg

It is surrounded by steep rock walls {{convert|600|m|abbr=on}} high, having been carved from the surrounding plateau by glaciers. After the glaciers melted, the land rebounded and the fjord was cut off from the sea. Salty water was eventually flushed from the fjord leaving it fresh. The catchment area is composed of igneous rock with relatively thin soil, so the waters feeding Western Brook Pond are low in nutrients and the lake is classified as ultraoligotrophic. It is fed by Stag Brook at the extreme eastern end of the lake and by numerous waterfalls cascading from the plateau above. One of these, Pissing Mare Falls at {{convert|350|m|abbr=on}}, is one of the highest in eastern North America.

The lake is accessible by a moderate-easy {{convert|3|km|abbr=on}} hiking trail over coastal bogs and low limestone ridges.{{cite web

| last =

| first =

| authorlink =

| title = Activities in Gros Morne National Park: Hiking

| work =

| publisher = Parks Canada

| url = http://www.pc.gc.ca/pn-np/nl/grosmorne/activ/activ2d_E.asp#Q

| format =

| doi =

| accessdate =2008-03-05 }} Two tour boats, one with a capacity of 70 passengers and the other 90 passengers, cruise the lake from June to mid-October.{{cite web

| last =

| first =

| authorlink =

| title = Activities in Gros Morne National Park: Boat tours

| work =

| publisher = Parks Canada

| url = http://www.pc.gc.ca/pn-np/nl/grosmorne/activ/activ2b_E.asp

| format =

| doi =

| accessdate =2008-03-05 }} The lake waters are pristine, having had very little impact from human activities. The tour boat operators had to undergo special certification to ensure that their operations would have minimal impact on the environment.[http://www.scc.ca/en/news-events/features/features-newfoundland-sightseeing-company-takes-iso-14001-on-tour Boat tour ISO14001 certification]

In the early part of the 20th century, a part of the surrounding cliff broke off and fell into the lake, causing a {{convert|30|m|abbr=on}} tsunami.{{cite web

| last = Ruffman

| first = Alan

| authorlink =

|author2=P.Geo

| title = Atlantic Tsunamis: "Like a River Returning"

| work =

| publisher = Maritime Museum of the Atlantic

| url = http://maritimemuseum.novascotia.ca/research/atlantic-tsunamis

| doi =

| accessdate =2014-05-04 }}

{{clear}}

See also

References