Pasadena orogeny is a mountain building event in the Western United States. Conventionally it refers to the formation of mountains in mainly Southern California during the Pleistocene and lasting until the present day; originally it referred to the uplift of the San Gabriel Mountains.
The Pasadena orogeny is a major Late Quaternary [1]-modern event [2] of mountain formation, [1] which took place in the middle or perhaps late Pleistocene [3] or to the present-day. [4] It is also known as the "Coast Ranges orogeny" [3] or considered to be part of the Cascadian orogeny [5] or Alpide Orogeny. [6] Finally, the term "Pasadena orogeny" is sometimes applied to all very recent orogenies around the Pacific Ocean. [7] The type location is close to Pasadena, California in the Transverse Ranges, [8] and originally referred to the fast rise of the San Gabriel Mountains recorded there. [9]
During this orogeny mountain ranges such as the San Bernardino Mountains, San Gabriel Mountains, San Jacinto Mountains, Santa Monica Mountains, Santa Ynez Mountains [10] and the Transverse Ranges grew, [11] as did the northern Channel Islands [10] such as Catalina Island and San Clemente Island, [12] the Kettleman Hills anticline in the San Joaquin Valley [13] and the Palos Verdes Hills. [14] [12] Sometimes the concept is limited to the uplift of the Transverse Ranges. [15]
The general uplift of mountains over a length of over 400 kilometres (250 mi) is caused by the collision of the North American Plate with other geologic structures that are attached to the Pacific Plate. [10] This orogeny has resulted in the uplift of mostly north-south trending mountain chains, although some east-west trending uplifts are also found such as the Channel Islands and the Transverse Ranges; [13] much of the uplift took place at the edge of basins. [16] The Pasadena orogeny is accompanied by earthquake activity, which includes tsunami hazards. [17]
Folding accompanying the uplift of the Coast Ranges in Southern California, [3] folding farther north at Morro Bay [18] and the structure of the Santa Barbara Basin [1] and Ventura Basin are consequences of the Pasadena orogeny. [4] The city of Long Beach, California lies within the affected region. [2]
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link)Pasadena orogeny is a mountain building event in the Western United States. Conventionally it refers to the formation of mountains in mainly Southern California during the Pleistocene and lasting until the present day; originally it referred to the uplift of the San Gabriel Mountains.
The Pasadena orogeny is a major Late Quaternary [1]-modern event [2] of mountain formation, [1] which took place in the middle or perhaps late Pleistocene [3] or to the present-day. [4] It is also known as the "Coast Ranges orogeny" [3] or considered to be part of the Cascadian orogeny [5] or Alpide Orogeny. [6] Finally, the term "Pasadena orogeny" is sometimes applied to all very recent orogenies around the Pacific Ocean. [7] The type location is close to Pasadena, California in the Transverse Ranges, [8] and originally referred to the fast rise of the San Gabriel Mountains recorded there. [9]
During this orogeny mountain ranges such as the San Bernardino Mountains, San Gabriel Mountains, San Jacinto Mountains, Santa Monica Mountains, Santa Ynez Mountains [10] and the Transverse Ranges grew, [11] as did the northern Channel Islands [10] such as Catalina Island and San Clemente Island, [12] the Kettleman Hills anticline in the San Joaquin Valley [13] and the Palos Verdes Hills. [14] [12] Sometimes the concept is limited to the uplift of the Transverse Ranges. [15]
The general uplift of mountains over a length of over 400 kilometres (250 mi) is caused by the collision of the North American Plate with other geologic structures that are attached to the Pacific Plate. [10] This orogeny has resulted in the uplift of mostly north-south trending mountain chains, although some east-west trending uplifts are also found such as the Channel Islands and the Transverse Ranges; [13] much of the uplift took place at the edge of basins. [16] The Pasadena orogeny is accompanied by earthquake activity, which includes tsunami hazards. [17]
Folding accompanying the uplift of the Coast Ranges in Southern California, [3] folding farther north at Morro Bay [18] and the structure of the Santa Barbara Basin [1] and Ventura Basin are consequences of the Pasadena orogeny. [4] The city of Long Beach, California lies within the affected region. [2]
{{
cite book}}
: |journal=
ignored (
help)
{{
cite book}}
: CS1 maint: location missing publisher (
link)