Post by jo on Feb 17, 2016 21:49:27 GMT -5
I have been wondering why ALBUQUERQUE ( New Mexico) has been chosen as a filming locale for WOLVERINE 3.
en.wikipedia.org/wiki/Albuquerque,_New_Mexico
Here's an interesting description of the incentives for filming in this city which is fairly close to the border between the USA and Mexico itself --
www.visitalbuquerque.org/albuquerque/film-tourism/
And does the area's physical characteristics give any hints as to the story veins that will be mined from the comic books? There seems to be such a picturesque image of the area surrounding the city itself.
A storyline derivative from OLD MAN LOGAN ? Of course that is just a guess although Hugh has dropped hints of OLD MAN LOGAN in the past as a possible storyline. Here's a summary of the story of OLD MAN LOGAN.
en.wikipedia.org/wiki/Old_Man_Logan
Jo
en.wikipedia.org/wiki/Albuquerque,_New_Mexico
Here's an interesting description of the incentives for filming in this city which is fairly close to the border between the USA and Mexico itself --
www.visitalbuquerque.org/albuquerque/film-tourism/
And does the area's physical characteristics give any hints as to the story veins that will be mined from the comic books? There seems to be such a picturesque image of the area surrounding the city itself.
Geography[edit]
Satellite image of Albuquerque taken by NASA.
According to the United States Census Bureau, Albuquerque has a total area of 189.5 square miles (490.9 km2), of which 187.7 square miles (486.2 km2) is land and 1.8 square miles (4.7 km2), or 0.96%, is water.[24]
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.[25][26] 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.
Geology[edit]
Albuquerque lies in the Albuquerque Basin, a portion of the Rio Grande rift.[27] 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."[28] He also notes that the Sandia Pueblo Indians call the mountain Bien Mur, "big mountain."[28]
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 calcium carbonate deposit common in the arid southwestern USA), along with some exposed granite bedrock.
Below the foothills, the area usually called the "Northeast 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 "West Bluff", 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.
Landscape[edit]
A panoramic view of the city of Albuquerque.
Satellite image of Albuquerque taken by NASA.
According to the United States Census Bureau, Albuquerque has a total area of 189.5 square miles (490.9 km2), of which 187.7 square miles (486.2 km2) is land and 1.8 square miles (4.7 km2), or 0.96%, is water.[24]
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.[25][26] 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.
Geology[edit]
Albuquerque lies in the Albuquerque Basin, a portion of the Rio Grande rift.[27] 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."[28] He also notes that the Sandia Pueblo Indians call the mountain Bien Mur, "big mountain."[28]
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 calcium carbonate deposit common in the arid southwestern USA), along with some exposed granite bedrock.
Below the foothills, the area usually called the "Northeast 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 "West Bluff", 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.
Landscape[edit]
A panoramic view of the city of Albuquerque.
A storyline derivative from OLD MAN LOGAN ? Of course that is just a guess although Hugh has dropped hints of OLD MAN LOGAN in the past as a possible storyline. Here's a summary of the story of OLD MAN LOGAN.
en.wikipedia.org/wiki/Old_Man_Logan
Jo
