Faralli

Adrienne M Faralli, age 43, Devon, PA View Details

Cities: Devon PA, Pottstown PA, Philadelphia PA Possible Relatives: Lisa Michele Cappelletti, Mary Ann Cappelletti, Matthew J Cappelletti

Anthony J Faralli, age 100, Wildwood, NJ View Details

Cities: Wildwood NJ, Philadelphia PA Possible Relatives: Carmen S Faralli, Frank R Faralli, Immacol Faralli

Anthony W Faralli, age 56, Wenonah, NJ View Details

Cities: Wenonah NJ, Winter Haven FL, Orange Park FL Possible Relatives: Walter Buzz Anthony, Alissa M Faralli, Anthony W Faralli

Allison Marlene Faralli, age 44, Woodbine, NJ View Details

Cities: Woodbine NJ, Corbin City NJ Possible Relatives: Corazon D Faralli, Mark T Faralli, Sofia A Faralli

Anthony J Faralli, age 65, Sewell, NJ View Details

Cities: Sewell NJ, Naples FL Possible Relatives: Maria E Bozzi, Anthony J Faralli, Christine Marie Faralli

Alexandria D Faralli, Wenonah, NJ View Details

Cities: Wenonah NJ Possible Relatives: W Faralli Anthony, Anthony W Faralli, Christie Lynn Kowalski

Alexis Faralli, Berwyn, PA View Details

Cities: Berwyn PA

Roseann J Faralli, age 55, Brick, NJ View Details

Locations: Medford NJ, Marlton NJ Possible Relatives: Maria C Crossan, Christine C Faralli

Janet L Lore, age 55, Woodbine, NJ View Details

Locations: Medford NJ, Marlton NJ Possible Relatives: Maria C Crossan, Christine C Faralli

Michele F Zurzolo, age 48, Burlington, NJ View Details

Locations: Medford NJ, Marlton NJ Possible Relatives: Maria C Crossan, Christine C Faralli

Maryann Ann Faralli, age 48, Bear, DE View Details

Locations: Medford NJ, Marlton NJ Possible Relatives: Maria C Crossan, Christine C Faralli

Jennifer A Peterson, age 42, Madison, WI View Details

Locations: Medford NJ, Marlton NJ Possible Relatives: Maria C Crossan, Christine C Faralli

Lisa Kolb Faralli, age 42, Mobile, AL View Details

Locations: Medford NJ, Marlton NJ Possible Relatives: Maria C Crossan, Christine C Faralli

Scott Lewis Faralli, age 41, Madison, WI View Details

Locations: Medford NJ, Marlton NJ Possible Relatives: Maria C Crossan, Christine C Faralli

Farallon Plate

The Farallon Plate was an ancient oceanic plate. It formed one of the three main plates of Panthalassa, alongside the Phoenix Plate and Izanagi Plate, which were connected by a triple junction. The Faread more...rallon Plate began subducting under the west coast of the North American Plate—then located in modern Utah—as Pangaea broke apart and after the formation of the Pacific Plate at the centre of the triple junction during the Early Jurassic. It is named for the Farallon Islands, which are located just west of San Francisco, California.read less...

Farallon de Pajaros

Farallón de Pájaros, also known as Uracus or Urracas, is a small (2.3 km2) uninhabited volcanic island, the northernmost island in the Northern Mariana Islands chain.

Farallon de Medinilla

Farallon de Medinilla is an uninhabited small island in the Northern Mariana Islands in the Pacific Ocean. It is located 45 nautical miles (83 km) north of Saipan, and is the smallest island in theread more... archipelago. Politically, it is part of the Northern Islands Municipality.read less...

Farallon Steamship Disaster

The Farallon Steamship Disaster was the wreck of a wooden Alaska Steamship Company passenger liner, SS Farallon, that hit Black Reef in Cook Inlet in the Territory of Alaska on 5 January 1910. All on read more...board evacuated to a nearby island, where most had to survive for a month in a mid-winter climate before they were rescued. Six other survivors survived an attempt to row across Shelikof Strait in search of rescue for the stranded men.read less...

Farallón, Cayey, Puerto Rico

Farallón is a barrio in the municipality of Cayey, Puerto Rico. Its population in 2010 was 451.

Farallon Trench

The Farallon Trench was a subduction related tectonic formation located off the coast of the western California continental margin during the late to mid Cenozoic era, around 50 miles southeast of modread more...ern-day Monterey Bay. The time duration of subduction began from around 165 Ma when the Farallon Plate replaced the Mezcalera promontory, until the San Andreas Fault straightening around 35 Ma. As data accumulated over time, a common view developed that one large oceanic plate, the Farallon Plate, acted as a conveyor belt, conveying accreted terranes onto the North American west coast. As the continent overran the subducting Farallon Plate, the denser plate became subducted into the mantle below the continent. When the plates converged, the dense oceanic plate sank into the mantle to form a slab below the lighter continent. Rapid subduction under the southwestern North America continent began 40 to 60 million years ago (Ma), during the mid Paleocene to mid Eocene epochs. This convergent subduction margin created a distinctive geomorphologic feature called an oceanic trench, which occurs at a convergent plate boundaries as a heavy metal rich, lithospheric plate moves below a light silica rich continental plate. The trench marks the position at which the flexed subducting slab begins to descend beneath and deform the continental plate margin. By 43 Ma, during the Eocene, worldwide plate motions changed and the Pacific Plate began to move away from North America and subduction of the Farallon Plate slowed dramatically. By around 36 Ma, the easternmost part of the East Pacific Rise, located between the Pioneer and Murray fracture zones at that time, approached the trench and the young, hot, buoyant lithosphere appears to have clogged part of the subduction zone, resulting in widespread dramatic uplift on land. The eventual complete subduction of this plate, consequential contact of the Pacific Plate with the California continental margin, and creation of the Mendocino Triple Junction (MTJ), took place around 30 to 20 Ma. The partial complete subduction and division of the Farallon Plate by the Pacific Plate, created the Juan de Fuca Plate to the north and the Cocos Plate to the south. The final stages of the evolution of California's continental margin was the growth of the San Andreas transform fault system, which formed as the Pacific Plate came into contact with the continental margin and the MTJ was formed. As subduction of the Pacific Plate continued along this margin, and the contact zone grew, the San Andreas proportionally grew as well.read less...