Point Roberts, Washington

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Point Roberts
Nickname: The Point, Point Bob
Location of Point Roberts in Whatcom County and Washington
Location of Point Roberts in
Whatcom County and Washington
Coordinates: 49°0′0″N 123°3′53″W / 49, -123.06472
Country United States
State Washington
County Whatcom
Established June 15, 1846
Elevation ft (0 m)
Population (2000)[1]
 - Total 1,308
Time zone PST (UTC-8)
 - Summer (DST) PDT (UTC-7)
Area code(s) 360
Website: www.pointrobertschamber.com

Point Roberts is a small unincorporated community in Whatcom County, Washington, United States. A geopolitical oddity, it is a practical exclave of the United States, located on the southernmost tip of the Tsawwassen Peninsula, south of Delta, British Columbia, Canada.

Point Roberts can be reached from the rest of the United States only by traveling through Canada or crossing Boundary Bay. Other exclaves of this type include the Northwest Angle, Minnesota and Elm Point, Minnesota.

Contents

The first Europeans to see Point Roberts were members of George Vancouver's expedition of 17911795; he named the point after his friend Henry Roberts who had originally been given command of the expedition. Point Roberts assumed its present political status in 1846, when the Oregon Treaty extended the 49th parallel as the boundary between American and British territory from the Rocky Mountains to Georgia Strait.

The Spanish discovered it first but mistook it for an island. Vancouver realized it was a peninsula at roughly the same time the Spanish did. Point Roberts was originally called Isla de Zepeda ([1]).

Notice at the international boundary between Canada and the United States in Point Roberts
Notice at the international boundary between Canada and the United States in Point Roberts

After years of joint occupation of the disputed area between the Columbia River and Russian America known as the Oregon Country to the Americans, and as the Columbia District to the British, democrats within the United States American expansionists like U.S. Senator Edward Allen Hannegan of Indiana urged Polk to annex the entire Oregon Country up to latitude 54°40'N, as the Democrats had called for in the election "Fifty-Four Forty or Fight".

While his government asserted that the title of America to the entire territory was unquestionable, Polk and his secretary, James Buchanan made an offer of a boundary at 49 degrees with the line straight across Vancouver Island, with no commercial privilege to be granted to the British south of the line, with the exception of free ports on Vancouver Island. This offer was rejected by the British and withdrawn by the US shortly thereafter.

On April 18, 1846, notice was forwarded to London that the US Congress had adopted a joint resolution abrogating the treaty of 1827 which provided for joint occupancy.

The British emissary, Richard Packenham, had previously been advised that the last concession which could be expected of America was in bending the boundary at the 49th parallel around the lower end of Vancouver Island. Fort Victoria was viewed as the future center for settlements on the island. It was deemed necessary around this point in time to give up territory on the Lower Mainland to keep Vancouver Island part of British North America.

In June 1848, Lord Aberdeen, British Foreign Secretary, proposed a treaty making the 49th parallel the boundary to the sea, giving Great Britain the whole of Vancouver Island. The treaty was concluded on June 15, 1855.

Point Roberts is a U.S. quasi-exclave bordered by Canada and the waters of Boundary Bay. It is 22 mi (35 km) south of downtown Vancouver, British Columbia. Point Roberts is part of the U.S. because it lies south of the 49th parallel, the official latitude defining the Canada-US border in that area. (Due to inaccuracies in 19th-century surveying, the border actually lies some 200 metres north of the 49th parallel in this location.)

Point Roberts borders the municipality of Delta in British Columbia. Boundary Bay lies to the east of Point Roberts and the Strait of Georgia to the south and west. The peninsula is about 2 mi (3 km) from north to south and about 3 mi (5 km) from east to west. It has an area of 4.884 square miles (12.65 km²).

As of the US 2000 census, there were 1,308 people, 1,820 households, and 474 families residing in the CDP. There were 1,838 housing units. The racial makeup of the CDP was 75.1% White, 12.3% African American, 0.9% Native American, 3.6% Asian, 0.1% Pacific Islander, 5.5% from other races, and 2.4% from two or more races. Hispanic or Latino of any race were 12.5% of the population.

In the CDP the population was spread out with 22.1% under the age of 19, 2.2% from 20 to 24, 29.0% from 25 to 44, 32.0% from 45 to 64, and 14.7% who were 65 years of age or older. The median age was 43.2 years.

The median income for a household in the CDP was $36,146, and the median income for a family was $45,417.

The zip code is 98281.

In the summertime the majority of people living in Point Roberts are Canadians who use it as a cottage or holiday spot.

Point Roberts Primary School
Point Roberts Primary School

Point Roberts Primary School, the only school on the Point, is for K–second-grade pupils; older public school students must be taken by bus into British Columbia and back into the United States at the Blaine, Washington, border crossing; it is a 40-minute drive.

After the September 11, 2001, attacks, school transportation became a question, with large delays at the border crossings, however, school buses were regularly given right of way and the issue was averted. Similar trips are often required for residents who wish to obtain goods not available in the exclave.

The U.S. Customs and Immigration station at Point Roberts
The U.S. Customs and Immigration station at Point Roberts

The only authorized land access to Point Roberts is 56th Street, a major thoroughfare that runs through the community of Tsawwassen on the Canadian side of the border; southward, the road turns into Tyee Drive. Point Roberts also has a small airport and a large marina for air and water access.

Many of the area's businesses are geared toward recreational and weekend visitors from Greater Vancouver, especially those in search of cheap gasoline. The handful of area bars and nightclubs are popular with visiting Canadians (despite a 21 drinking age in the US versus 19 in British Columbia), and were even more so in the days before Sunday drinking was legalized in British Columbia. The local post office rents hundreds of post office boxes to individuals and businesses from the Greater Vancouver area (including the US Consulate in Vancouver) which find it a convenient and fast way to receive mail and parcels from the United States without paying for cross-border shipping costs.

As reported in National Geographic Magazine, residents enjoy a low crime rate at the cost of a high local security presence.

Extremely rare, but postcard-worthy snow fall
Extremely rare, but postcard-worthy snow fall

Also referred to as "The Point" and "Point Bob", Point Roberts lies within a Blue hole created by Vancouver Island, the north shore mountains surrounding Vancouver, and the North Cascades (including Mount Baker). This micro-climate provides some of the mildest weather in the Pacific Northwest. With an average annual rainfall of about 1000 mm (40 inches), Point Roberts enjoys more sunny days and a milder climate than its neighbors.

East cliff-face at Lily Point
East cliff-face at Lily Point

Beneath Point Roberts, the bedrock Chuckanut Formation was deposited as an alluvial plain containing layers of sediments consisting of silt, sand, sand and gravel, and peat. During the last 60 million years the sediments were compacted and folded by mountain building forces resulting from continental drift to form strata of siltstone, sandstone, conglomerate and coal. During recent geologic history, the Chuckanut formation was overridden by four or more glaciations. [2]

Point Roberts consists of a series of the resulting glacial sediments resting upon the Chuckanut Formation. The lowest glacial sediments (now near sea level) are from Salmon Springs or older glaciations. At the peak of the most recent glaciation, the main ice sheet was in excess of 7,000 feet thick as it moved southward between Vancouver Island and the Canadian Coast Range and down the Strait of Georgia. A smaller lobe of the continental glacier in excess of 5,000 feet traveled down the Fraser River flood plains merging with the main ice sheet over the greater Vancouver area and Whatcom and Skagit Counties. The coalesced continental ice sheet traveled south terminating in the vicinity of Chehalis, Washington. Relatively impermeable Vashon glacial lodgment till (estimated to be as much as 40 feet thick at the uppermost layer) was plastered over the advance outwash as the weight of the 7,000 foot thick plus Strait of Georgia ice lobe moved southward over approximately 10,000 years. (Armstrong, et. all, 1965) Point Roberts, Tsawwassen, and part of British Columbia extending Past English Bluff actually comprised an island at the close of the Vashon glaciation, approximately 11,000 years ago.

As the ice sheets melted, the thinner Fraser Lobe began to float while the Strait of Georgia lobe acted as a dam forming a lake under the Fraser Lobe. Sediments settling from the melting, floating ice resulted in the accumulation of 300 feet or more of Glacial Marine Drift over much of western Whatcom County. (Easterbrook, 1976; Geologic Map of Western Whatcom County, Washington, USGS, Map I-854-B) This Glacial Marine Drift is generally soft and was not consolidated by the weight of the glacier. A discontinuous, thin mantle of this Glacial Marine Drift above the Glacial Lodgment Till has been identified sporadically across Point Roberts. The uppermost layer of glacial sediments consists of recessional sand, silt, and gravel deposited as the Strait of Georgia ice lobe receded. Since the recession of the glaciers, the Fraser River has deposited deltaic sediments on the north and easterly side of the Point Roberts-Tsawwassen Island connecting it to the Greater Vancouver mainland. At some locations, these sediments have been eroded or removed exposing the lodgment till.

Sunset at Lighthouse Marine Park
Sunset at Lighthouse Marine Park
  • Maple Beach, Washington (NE)
  • Monument Park (NW)
  • Lighthouse Marine Park (SW)
  • Nature Trail (SW)
  • Point Roberts Skate Park (Central - recreational open space)
  • Lily Point (SE)
  • Cascadia Marine Trail (E)

Looking north towards British Columbia at low-tide from Maple Beach
Looking north towards British Columbia at low-tide from Maple Beach
  • Bells Grove
  • Crystal Waters
  • Freeman Beach
  • Lily Point
  • Maple Beach
  • Waters Plat

Until 1988, Point Roberts telephone numbers were in British Columbia's 604 area code and served by BCTel, a Canadian telephone company. Today, Point Roberts phone numbers are in the 360 area code and the 945 exchange, and the local regular-service telecom provider is Whidbey Island Telephone Company. Point Roberts is served by DirectTV and Delta Cablevision for cable TV and broadband internet. Mobile telephone service is provided by a variety of companies, both American and Canadian.

Mount Baker, as seen across Boundary Bay
Mount Baker, as seen across Boundary Bay

  1. ^ Point Roberts Demographic Information. Point Roberts Chamber of Commerce (2000). Retrieved on 2007-10-18.
  2. ^ Armstrong, J.E; D.R. Crandell, D.J. Easterbrook, J.B. Noble (March 1965). "Late Pleistocene Stratigraphy and Chronology in Southwestern British Columbia and Northwestern Washington". Geological Society of America Bulletin 76: 321–330. 


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