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Albuquerque
New Mexico United States
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Excel Manufacturing, Inc.
9916 Cochiti Rd SE Albuquerque, NM 87123
(505) 271-8858
     
Talent Pool
4004 Palacio Real Avenue Northwest, Albuquerque, NM 87120
(505) 898-0661
Billy's Long Bar
4800 San Mateo Boulevard Northeast, Albuquerque, NM 87109-2424
(505) 889-0573
Blue Jeans Lounge
9018 Central Avenue Southeast, Albuquerque, NM 87123-2508
(505) 294-8138
Grandma's Music & Sound
9310 Coors Boulevard Northwest, Albuquerque, NM 87114-4006
(505) 292-0341
Kellys Brewery
3222 Central Ave SE, Albuquerque, NM 87106
(435) 538-7911
Tom Quirk Automotive
3434 Girard Boulevard Northeast, Albuquerque, NM 87107-1929
(505) 883-0793
Budget: Albuquerque North Northeast
2500 San Mateo Boulevard Northeast, Albuquerque, NM 87110-4055
(505) 830-6953
Amway Products Distributors
2613 Fantozzi Road Southwest, Albuquerque, NM 87105-5731
(505) 877-6654
Debonair Real Estate
2920 Carlisle Boulevard Northeast, Albuquerque, NM 87110-2867
(505) 888-7673
 
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City Overview

Albuquerque (pronounced /ˈælbəkɜrkiː/; Spanish pronunciation: [alβuˈkerke]; known as Bee'eldííldahsinil in Navajo) is the largest city in the state of New Mexico, United States. It is the county seat of Bernalillo County and is situated in the central part of the state, straddling the Rio Grande. The city population was 521,999 as of July 1, 2008, according to U.S. census estimates, and ranks as the 34th-largest city in the U.S. As of June 2007, the city was the 6th fastest growing in America. With a metropolitan population of 845,913 as of July 1, 2008, Albuquerque is the 59th-largest United States metropolitan area. The Albuquerque MSA population includes the city of Rio Rancho, one of the fastest growing cities in the United States. Roughly half of the population of the state of New Mexico lives in the Albuquerque area.

Albuquerque is home to the University of New Mexico (UNM), Kirtland Air Force Base, Sandia National Laboratories, Lovelace Respiratory Research Institute, and Petroglyph National Monument. The Sandia Mountains run along the eastern side of Albuquerque, and the Rio Grande flows through the city, north to south.

History

Early settlers

The city was founded in 1706 as the Spanish colonial outpost of Ranchos de Alburquerque; present-day Albuquerque retains much of the Spanish cultural and historical heritage.

Albuquerque was a farming community and strategically located military outpost along the Camino Real. The town of Alburquerque was built in the traditional Spanish village pattern: a central plaza surrounded by government buildings, homes, and a church. This central plaza area has been preserved and is open to the public as a museum, cultural area, and center of commerce. It is referred to as "Old Town Albuquerque" or simply "Old Town." "Old Town" was sometimes referred to as "La Placita" ("little plaza" in Spanish).

The village was named by the provincial governor Don Francisco Cuervo y Valdes in honour of Don Francisco Fernández de la Cueva, viceroy of New Spain from 1653 to 1660. One of de la Cueva's aristocratic titles was Duke of Alburquerque, referring to the Spanish town of Alburquerque.

The Alburquerque family name dates from pre-12th century Iberia (Spain and Portugal) and is habitational in nature (de Alburquerque = from Alburquerque). The Spanish village of Alburquerque is within the Badajoz province of Extremadura region, and located just fifteen miles (24 km) from the Portuguese border. Cork trees dominate the landscape and Alburquerque is a center of the Spanish cork industry. Over the years, this region has been alternately under both Spanish and Portuguese rule. It is interesting to note that the name of the New Mexico city of Albuquerque follows the Portuguese spelling with only one 'r'. Historically, the land around Alburquerque was invaded and settled by the Moors (711 AD) and the Romans (218 BC) before them. Thus, the word Alburquerque may be rooted in the Arabic (Moorish) 'Abu al-Qurq', which means "father of the cork oak", or "land of the cork oak" (the land as father – fatherland). Alternately, it may be Latin (Roman) in origin and from 'albus quercus' or "white oak" (the wood of the cork oak is white after the bark has been removed). The seal of the Spanish village of Alburquerque is a white oak tree, framed by a shield, topped by a crown.

Spain established a Presidio in Albuquerque from 1706. After 1821, Mexico also had a military garrison there.

Following the American occupation of New Mexico, Albuquerque had a Federal garrison and quartermaster depot, the Post of Albuquerque, from 1846 to 1867. During the Civil War Albuquerque was occupied in February 1862 by Confederate troops under General Henry Hopkins Sibley, who soon afterwards advanced with his main body into northern New Mexico. During his retreat from Union troops into Texas he made a stand on April 8, 1862, at Albuquerque and fought the Battle of Albuquerque against a detachment of Union soldiers commanded by Colonel Edward R. S. Canby. This day-long engagement at long range led to few casualties.

When the Atchison, Topeka and Santa Fe Railroad arrived in 1880, it bypassed the Plaza, locating the passenger depot and railyards about 2 miles (3 km) east in what quickly became known as New Albuquerque or New Town. To quell its then rising violent crime rate, gunman Milt Yarberry was appointed the town's first Marshal that same year. New Albuquerque was incorporated as a town in 1885, with Henry N. Jaffa its first mayor, and incorporated as a city in 1891.:232–233 Old Town remained a separate community until the 1920s when it was absorbed by the City of Albuquerque. Albuquerque High School, the city's first public high school, was established in 1879.

Early 20th century

New Albuquerque quickly became a tidy southwestern town which by 1900 boasted a population of 8,000 inhabitants and all the modern amenities including an electric street railway connecting Old Town, New Town, and the recently established UNM campus on the East Mesa. In 1902 the famous Alvarado Hotel was built adjacent to the new passenger depot and remained a symbol of the city until it was torn down in 1970 to make room for a parking lot. In 2002, the Alvarado Transportation Center was built on the site in a manner resembling the old landmark. The large metro station functions as the downtown headquarters for the city's transit department, and serves as an intermodal hub for local buses, Greyhound buses, Amtrak passenger trains, and the Rail Runner commuter rail line.

New Mexico's dry climate brought many tuberculosis patients to the city in search of a cure during the early 1900s, and several sanitaria sprang up on the West Mesa to serve them. Presbyterian Hospital and St. Joseph Hospital, two of the largest hospitals in the Southwest, had their beginnings during this period. Influential New Deal-era governor Clyde Tingley and famed southwestern architect John Gaw Meem were among those brought to New Mexico by tuberculosis.

Decades of growth

In June 2007, Albuquerque was listed as the 6th fastest growing city in America by CNN and the US Census Bureau.

The first travelers on Route 66 appeared in Albuquerque in 1926, and before long, dozens of motels, restaurants, and gift shops had sprung up along the roadside to serve them. Route 66 originally ran through the city on a north-south alignment along Fourth Street, but in 1937 it was realigned along Central Avenue, a more direct east-west route. The intersection of Fourth and Central downtown was the principal crossroads of the city for decades. The majority of the surviving structures from the Route 66 era are on Central, though there are also some on Fourth. Signs between Bernalillo and Los Lunas along the old route now have brown, historical highway markers denoting it as Pre-1937 Route 66.

The establishment of Kirtland Air Force Base in 1939, Sandia Base in the early 1940s, and Sandia National Laboratories in 1949, would make Albuquerque a key player of the Atomic Age. Meanwhile, the city continued to expand outward onto the West Mesa, reaching a population of 201,189 by 1960. In 1990 it was 384,736 and in 2007 it was 518,271.

Albuquerque's downtown entered the same phase and development (decline, "urban renewal" with continued decline, and gentrification) as nearly every city across the United States. As Albuquerque spread outward, the downtown area fell into a decline. Many historic buildings were razed in the 1960s and 1970s to make way for new plazas, high-rises, and parking lots as part of the city's urban renewal phase. Only recently has downtown come to regain much of its urban character, mainly through the construction of many new loft apartment buildings and the renovation of historic structures like the KiMo Theater, in the gentrification phase.

New millennium

During the 21st century, the Albuquerque population has continued to grow rapidly. The population of the city proper is estimated at 521,999 in 2008, up from 448,607 in the 2000 census. The metropolitan area population is estimated at 845,913 in 2008, up from 729,649 in the 2000 census.

During 2005 and 2006, the city celebrated its tricentennial with a diverse program of cultural events.

Mesa del Sol is a new large master-planned community currently being developed in Albuquerque, that is projected to bring in 100,000 residents and 40,000 more jobs.

Urban trends and issues

Government leaders and many citizens in the city have actively pursued urban projects taken on by cities many times larger. This has resulted in the successful revitalization of downtown, creating restaurants, offices, and residential lofts. The strip of Central Avenue between First and Eighth streets has become a hub of urban life. Alvarado Station provides convenient access to other parts of the city via ABQ RIDE, the city bus system. The city wants to provide better public transportation opportunities to ease the city's growing traffic woes. A street car is being considered and would initially extend up the Central Avenue corridor from the westside, through downtown, past UNM and the Nob Hill district, and into the Uptown Area.

Many citizens fear Albuquerque may be growing beyond its means. A majority of residents want to avoid increasing crime and traffic, worsening air quality, stressing water supplies, and encroaching on the natural environment. Many feel these are the negative consequences of persistent sprawl development patterns.

On March 23, 2007, the city's mayor Martin Chavez announced his plan to brand the city "the Q". Despite various opinions as to what the city's nickname should be, Mayor Chavez is continuing to push his initiative.

Soy de Burque, "I am from Burque", is one response to the mayor's vision of a "hip" reincarnation". This group of Albuquerque’s residents feels it is unnecessary to spend taxpayer money to hire marketing companies to brand their city with a more palatable nickname, recognizing the city already has a brand and nickname. This selling of a city’s cultural identity to marketing and advertising firms to brand and sell has been dubbed by Soy de Burque as culture branding. One central issue to their response is the branding campaign was never voted on, but rather declared by Mayor Chavez, and outsourced to marketing and advertising firms.

The passage of the Planned Growth Strategy in 2002–2004 marked the community's strongest effort to create a framework for a more balanced and sustainable approach to urban growth.

"A critical finding of the study is that many of the 'disconnects' between the public's preferences and what actually is taking place are caused by weak or non-existent implementation tools - rather than by inadequate policies, as contained in the City/County Comprehensive Plan and other already adopted legislation."

Urban sprawl is limited on three sides by the Pueblo of Sandia to the north, the Pueblo of Isleta and Kirtland Air Force Base to the south, and the Sandia Mountains to the east. Suburban growth continues at a strong pace to the west beyond the Petroglyph National Monument, once thought to be a natural boundary to sprawl development.

Because of cheaper land and lower taxes, much of the growth in the metropolitan area is taking place outside of the City of Albuquerque itself. In Rio Rancho to the northwest, the communities east of the mountains, and the incorporated parts of Valencia County, population growth rates approach twice that of the city. The primary cities in Valencia County are Los Lunas and Belen, both of which are home to growing industrial complexes and new residential subdivisions. The Mid Region Council of Governments (MRCOG), which includes constituents from throughout the Albuquerque area, was formed to insure that these governments along the middle Rio Grande would be able to meet the needs of their rapidly rising populations. MRCOG's cornerstone project is the New Mexico Rail Runner Express.

Geography

According to the United States Census Bureau, Albuquerque has a total area of 181.3 square miles (469.6 km²). 180.6 square miles (467.8 km²) of it is land and 0.6 square miles (1.6 km²) of it (0.35%) is water. The metro area has over 1,000 square miles (2,600 km2) developed.

Albuquerque lies within the northern, upper edges of the Chihuahuan Desert ecoregion, based on long-term patterns of climate, associations of plants and wildlife, and landforms, including drainage patterns. Located in central New Mexico, the city also has noticeable influences from the adjacent Colorado Plateau Semi-Desert, Arizona-New Mexico Mountains, and Southwest Plateaus and Plains Steppe ecoregions, depending on where one is located. Its main geographic connection lies with southern New Mexico, while culturally, Albuquerque is a crossroads of most of New Mexico.

Albuquerque has one of the highest elevations of any major city in the United States, though the effects of this are greatly tempered by its southwesterly continental position. The elevation of the city ranges from 4,900 feet (1,490 m) above sea level near the Rio Grande (in the Valley) to over 6,700 feet (1,950 m) in the foothill areas of Sandia Heights and Glenwood Hills. At the airport, the elevation is 5,352 feet (1,631 m) above sea level.

The Rio Grande is classified, like the Nile, as an 'exotic' river because it flows through a desert. The New Mexico portion of the Rio Grande lies within the Rio Grande Rift Valley, bordered by a system of faults, including those that lifted up the adjacent Sandia and Manzano Mountains, while lowering the area where the life-sustaining Rio Grande now flows.

Albuquerque is located at 35°6′39″N 106°36′36″W / 35.11083°N 106.61°W / 35.11083; -106.61 (35.110703, -106.609991).

Climate

Albuquerque's climate is usually sunny and dry, with low relative humidity. Brilliant sunshine defines the region, averaging more than 300 days a year; periods of variably mid and high-level cloudiness temper the sun at other times. Extended cloudiness is rare. The city has four distinct seasons, but the heat and cold are mild compared to the extremes that occur more commonly in other parts of the country.

Winters are rather brief but definite; daytime highs range from the mid 40s to upper 50s Fahrenheit, while the overnight lows drop into the low 20s to near 30 by sunrise; nights are often colder in the valley and uppermost foothills by several degrees, or during cold frontal passages from the Great Basin or Rocky Mountains. The occasional snowfall, associated with low pressure areas, fronts and troughs, often melts by the mid-afternoon; over half of the scant winter moisture occurs in the form of light rain showers, usually brief in duration. In the much higher and colder Sandia Mountains, moisture falls as snow; many years have enough snow to create decent skiing conditions at the local ski area.

Spring time starts off windy and cool, sometimes unsettled with some rain and even light snow, though spring is usually the driest part of the year in Albuquerque. March and April tend to see many days with the wind blowing at 20 to 30 mph (32 to 48 km/h), and afternoon gusts can produce periods of blowing sand and dust. In May, the winds tend to subside, as temperatures start to feel like summer.

Summer daytime highs range from the upper 80s to the upper 90's, while dropping into the low 60s to low 70s overnight; the valley and uppermost foothills are often several degrees cooler than that. The heat is quite tolerable because of low humidity, except during the late summer during increased humidity from surges in the monsoonal pattern; at that time, daytime highs drop slightly but the extra moisture in the air can cause nighttime temperatures to increase.

Fall sees mild days and cool nights with less rain, though the weather can be more unsettled closer to winter.

The city was one of several in the region experiencing a severe winter storm on December 28–30, 2006, with locations in Albuquerque receiving between 10.5 and 26 inches (27 and 66 cm) of snow.

Albuquerque's climate is classified as arid (BWk or BWh, depending on the particular scheme of the Köppen climate classification system one uses), meaning average annual precipitation is less than half of evaporation, and the mean temperature of the coldest month is above freezing (32F). Only the wettest areas of the Sandia foothills are barely semi-arid, where precipitation is more than half of, but still less than, evaporation; such areas are localized and usually lie above 6,000 feet (1,800 m) in elevation and often in arroyo drainages, signified by a slightly denser, taller growth of evergreen oak–juniper–pinon chaparral and rarely, woodland, often mixed with taller desert grasses. These elevated foothill areas still border arid areas, best described as desert grassland or desert shrub, on their west sides.

Traveling to the west, north and east of Albuquerque, one quickly rises in elevation and leaves the sheltering effect of the valley to enter a noticeably cooler and slightly wetter environment. One such area is still considered part of metro Albuquerque, commonly called the "East Mountain" area; it is covered in savannas or woodlands of low juniper and pinon trees, reminiscent of the lower parts of the southern Rocky Mountains, which do not actually contact Albuquerque proper.

Those mountains and highlands beyond the city create a "rain shadow" effect, due to the drying of descending air movements; the city usually receives very little rain or snow, averaging 8–9 inches (216 mm) of precipitation per year. Valley and west mesa areas, farther from the mountains are drier, averaging 6–8 inches of annual precipitation; the Sandia foothills tend to lift any available moisture, enhancing precipitation to about 10–17 inches annually. Most precipitation occurs during the summer monsoon season (also called a chubasco in Mexico), typically starting in early July and ending in mid-September.

Geology

The Sandia Mountains are the predominant geographic feature visible in Albuquerque. "Sandía" is Spanish for "watermelon", and is popularly believed to be a reference to the brilliant coloration of the mountains at sunset: bright pink (melon meat) and green (melon rind). The pink is due to large exposures of granodiorite cliffs, and the green is due to large swaths of conifer forests. However, Robert Julyan notes in The Place Names of New Mexico, "the most likely explanation is the one believed by the Sandia Pueblo Indians: the Spaniards, when they encountered the Pueblo in 1540, called it Sandia, because they thought the squash growing there were watermelons, and the name Sandia soon was transferred to the mountains east of the pueblo." He also notes that the Sandia Pueblo Indians call the mountain Bien Mur, "big mountain."

The Sandia foothills, on the west side of the mountains, have soils derived from that same rock material with varying sizes of decomposed granite, mixed with areas of clay and caliche (a calcareous clay common in the arid southwestern USA), along with some exposed granite bedrock.

Below the foothills, the area usually called the "Heights" consists of a mix of clay and caliche soils, overlain by a layer of decomposed granite, resulting from long-term outwash of that material from the adjacent mountains. This bajada is quite noticeable when driving into Albuquerque from the north or south, due to its fairly uniform slope from the mountains' edge downhill to the valley. Sand hills are scattered along the I-25 corridor and directly above the Rio Grande valley, forming the lower end of the Heights.

The Rio Grande valley, due to long-term shifting of the actual river channel, contains layers and areas of soils varying between caliche, clay, loam, and even some sand. It is the only part of Albuquerque where the water table often lies close to the surface, sometimes less than 10 feet (3.0 m).

The last significant area of Albuquerque geologically is the West Mesa: this is the elevated land west of the Rio Grande, including the sandy terrace immediately west and above the river, and the rather sharply defined volcanic escarpment above and west of most of the developed city. The west mesa commonly has soils often referred to as "blow sand", along with occasional clay and caliche and even basalt, nearing the escarpment.

Hydrology

Albuquerque's drinking water presently comes from a delicate aquifer that was once described as an "underground Lake Superior". The Albuquerque Bernalillo County Water Utility Authority (ABCWUA) has developed a water resources management strategy, which pursues conservation and the direct extraction of water from the Rio Grande for the development of a stable underground aquifer in the future.

The aquifer of the Rio Puerco is too saline to cost-effectively use for drinking purposes.

Much of the rainwater that Albuquerque receives does not recharge its aquifer. It is diverted through storm drains called arroyos, to the Rio Grande. The water flowing in the Rio Grande was thought to recharge Albuquerque's aquifer, however, it is actually separated from the rest of the water table.

Of the 62,780 acre feet (77,440,000 m3) per year of the water in the upper Colorado River basin entitled to municipalities in New Mexico by the Upper Colorado River Basin Compact, Albuquerque owns 48,200. The water is delivered to the Rio Grande by the San JuanChama Project. The project's construction was initiated by legislation enacted by President John F. Kennedy in 1962, and completed in 1971. This diversion project transports water under the continental divide from Navajo Lake to Lake Heron on the Rio Chama, a tributary of the Rio grande. Presently, this water is resold to downstream owners in Texas. These arrangements will end in 2008 with the completion of the ABCWUA's Drinking Water Supply Project.

This project will, using a system of adjustable height dams, skim water from the Rio Grande into sluices which will lead to water treatment facilities for direct conversion to potable water. Some water will be allowed to flow through central Albuquerque, mostly to protect the endangered Rio Grande Silvery Minnow. Treated effluent water will be recycled into the Rio Grande to the South of the city. The ABCWUA expects river water to comprise up to seventy percent of its water budget in 2060. Groundwater will still be used. One of the policies of the ABCWUA's strategy is the acquisition of additional river water. :Policy G, 14

Source: http://en.wikipedia.org/wiki/Albuquerque,_New_Mexico


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