The Cordillera Blanca fault zone is a major west dipping normal fault that bounds the west side of a 120- to 170-km-wide zone of active extension along the crest of the northern Peruvian Andes. The fault is approximately 210 km long and exhibits continuous geomorphic evidence of repeated late Pleistocene and Holocene displacements but has not been the source of historical or teleseismically recorded earthquakes. Trenching and mapping of fault scarps provide new information on earthquake recurrence, slip rate, timing of the most recent events, and Andean neotectonics.

At Quebrada Queroccocha, 55 km from the south end of the zone, an 11,000- to 14,000-year-old moraine is displaced 12--15 m, and younger valley fill lacustrine and fluvial deposits are displaced 7.5--8 m. Scarp profiles, tectonic terraces, and trench exposures indicate five to seven scarp-forming earthquakes of 2--3 m per event during the past 11,000--14,000 years at this location. Considering uncertainties in the number of events and in the age of the displaced moraine, the average recurrence interval is estimated to be 2440¿1060 years. Detrital charcoal from colluviums that predate and postdate the most recent event yielded ages of 2480¿65 and 750¿80 14C years B.P., respectively, and stratigraphic relationships suggest that the event may be closer to the older date. The late Quaternary slip rate at Quebrada Queroccocha is 0.86--1.36 mm/yr and appears to be representative of much of the fault zone. At Pachma Bajo, located 30 km from the north end of the zone on a separate segment, displacement during each of the past two events was 2 to ≥3 m.

The morphology of scarps in alluvial fan and debris flow deposits indicates recurrence intervals of about 1000--3000 years. Relationships between pre-Inca walls and faulted deposits suggest that 1500--2000 years have elapsed since the most recent event. Fault behavior parameters, particularly displacement per event and fault segment length, show that the Cordillera Blanca fault zone is similar to seismogenic normal faults that nucleate M 7--7 1/2 earthquakes at depths of approximately 15 km. The Quebrada Queroccocha slip rate and analysis of other normal faults in the region suggest cumulative late Quaternary extensional strain rates of about 1--4 mm/yr across the complete zone of Andean crestal extension.