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Loch Lomond

New Brunswickvillage

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Elevation79 m
Land area71 km²
Coordinates45.35°, -65.87°

Demographic figures from Statistics Canada. Overview below cites Wikipedia and may reference a different year.

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City facts

Elevation
79 m
Area
71 km²

Facts from Wikidata (CC0).

Overview

Situated in New Brunswick, Canada, Loch Lomond is a village. Detailed population figures are not currently catalogued in the open data sources we track. On the world map it falls within the Western Hemisphere, specifically at 45.353°, -65.869°. Solar-resource estimates put the area at about 1,275 kWh/m² of solar irradiance per year with sunshine for roughly 50% of daylight hours. The latitude suggests four distinct seasons with warm summers and cold winters. Further detail — demographics, climate, nearby amenities and natural-hazard data — is compiled below from public open-data sources.

Summary composed automatically from structured open data on this page. See our Terms for details.

History & geography

History

People first arrived in the Loch Lomond area around 5000 years ago, during the Neolithic era. They left traces of their presence at places around the loch, including Balmaha, Luss, and Inchlonaig. were built at points in the loch. The crannog known as "The Kitchen", located off the island of Clairinsh, may have later been used as a place for important meetings by Clan Buchanan whose clan seat had been on Clairinsh since 1225: this usage would be in line with other crannogs such as that at Finlaggan on Islay, used by Clan Donald. During the Early Medieval period viking raiders sailed up Loch Long, hauled their longboats over at the narrow neck of land at Tarbet, and sacked several islands in the loch. Loch Lomond became a popular destination for travellers, such that when James Boswell and Samuel Johnson visited the islands of Loch Lomond on the return from their tour of the Western Isles in 1773, the area was already firmly enough established as a destination for Boswell to note that it would be unnecessary to attempt any description. The depression in which Loch Lomond lies was carved out by glaciers during the retreat of the last ice age, during a temporary return to glacial conditions known as the Younger Dryas. Locally this is known as the Loch Lomond Readvance, between 20,000 and 10,000 years ago. to create a narrow, fjord-like finger lake.This area is underlain by ancient Precambrian and Cambrian schists and quartzites, which contributed to the formation of the deep and narrow northern basin, reaching depths of up to 190 metres. Further south the glaciers were able to spread across the softer Lowland sandstone, leading to a wider body of water that is rarely more than 30 m deep. The southern part of the loch features younger Devonian sandstones and…

Excerpted from the corresponding Wikipedia article (CC BY-SA).

Geography

Latitude
45.3530
Longitude
-65.8691
Water area
—
View on OpenStreetMap

Coordinates & boundaries from the US Census TIGER/Line shapefiles.

Climate

Air quality

Walkability

Amenities nearby

Wildlife & biodiversity

Earthquake history

Photos

Sights & places nearby

Notable people from here

Geography & sun

Avg solar (kWh/m²/day)
3.49
Annual solar (kWh/m²)
1,275

Elevation, sunrise/sunset and daylight from Open-Meteo. Solar climatology from NASA POWER.

Nearby airports

Public attention

Wikipedia views (last 30 days)
9,235
Avg daily Wikipedia views
318
Attention level
Modest

Pageview totals from the Wikimedia Pageviews API.

Books about Loch Lomond

Search results from Open Library.

Recent natural events nearby

Ground air-quality sensors

Recently spotted species

Events

Notable, recurring, and historical events associated with Loch Lomond, sourced from Wikidata.

Source: Wikidata (CC0).

Sources

  • • Wikipedia
  • • Wikidata
  • • Open-Meteo / sunrise-sunset.org
  • • Wikipedia Pageviews API
  • • Open Library