Question: What fault zone traverses Central Park?
About the article "Central Park", section "Geology".

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The Hosgri Fault (also Hosgri Fault Zone, San Gregorio-Hosgri Fault Zone) is an offshore fault zone located near the Central Coast of California in San Luis Obispo County.
The main fault stretches for about , and the coastal communities closest to it are Cambria, San Simeon and Morro Bay, Baywood Park-Los Osos, and Avila Beach.
The fault system (including branches) is some 420 km long, and is a right-lateral strand of the San Andreas fault system. 
There are four different types of bedrock in Manhattan.
In Central Park, Manhattan schist and Hartland schist, which are both metamorphosed sedimentary rock, are exposed in various outcroppings.
The other two types, Fordham gneiss (an older deeper layer) and Inwood marble (metamorphosed limestone which overlays the gneiss), do not surface in the park.
Fordham gneiss, which consists of metamorphosed igneous rocks, was formed a billion years ago, during what is known as the Grenville orogeny that occurred during the creation of an ancient super-continent.
It is the oldest rock in the Canadian Shield, the most ancient part of the North American tectonic plate.
Manhattan schist and Hartland schist were formed in the Iapetus Ocean during the Taconic orogeny in the Paleozoic era, about 450 million years ago.
During this period the tectonic plates began to move toward each other, which resulted in the creation of the supercontinent, Pangaea.
Cameron's Line is a fault zone that traverses Central Park on an east-west axis.
Various glaciers have covered the area of Central Park in the past, with the most recent being the Wisconsin glacier which receded about 12,000 years ago.
Evidence of past glaciers are visible throughout the park in the form of "glacial erratics" (large boulders dropped by the receding glacier) and north-south glacial striations visible on stone outcroppings.
The following is a partial list of faults in Costa Rica: Agua Caliente Fault, in the Central Valley.
Alajuela Fault, in the Central Valley.
Ángel-Varablanca Fault, in the Central Valley.
Atirro Fault, in Turrialba.
Buenavista Fault, in Pérez Zeledón.
Canoas Fault, in the Southern Zone.
Chiripa Fault, in the Northern Zone.
Escazú Fault, in the Central Valley.
Golfito Fault, in Golfito.
Guápiles Fault, in Caribbean Zone.
Jateo Fault, in the Central Valley.
Navarro Fault, in Turrialba.
San Miguel Fault, in the Central Valley.
Zarceró Fault, in the Northern Zone.  
  Altai Mountains (Western Mongolia and Southern Siberia, Russia)  Western Aleutian Subduction Zone  Gobi Altai (Central Mongolia)  "Big Bend" of the San Andreas Fault Zone, (California, USA)  Alpine Fault in New Zealand  
The Highland Boundary Fault is a major fault zone that traverses Scotland from Arran and Helensburgh on the west coast to Stonehaven in the east.
It separates two distinctly different physiographic and geological terrains: the Highlands from the Lowlands, and in most places it is recognisable as a change in topography.
Where rivers cross the fault they often pass through gorges and the associated waterfalls can be a barrier to salmon migration.
The fault is believed to have formed in conjunction with the Strathmore Syncline to the south-east during the Acadian orogeny in a transpressive regime that caused the uplift of the Grampian block and a small sinistral movement on the Highland Boundary Fault.