Mountain building in the Andes, the longest continental mountain range on Earth, started in
the Late Cretaceous but was highly diachronous. Reconstructing the timing of surface uplift …

Miocene strike‐slip tectonics was responsible for creating and closing short‐lived (ca. 6 Ma)
passages and the emergence of isolated topography in the Northern Andes. These …

The construction and destruction of mountain belts exert a first-order control in ecosystems
by creating bridges and barriers for populations, modifying river-drainage networks and …

Some physically based landslide models analyse pore water pressure changes due to
rainfall infiltration and its effects on slope stability. The physically-based model TRIGRS has …

We explore the structural and geomorphological evidence for recent tectonic activity in the
Serranía de San Lucas (San Lucas Range, SLR), the northern segment of the Central …

New geochronologic, thermochronologic, and geomorphometric landscape analyses were
performed to discriminate the relationships between tectonics and geomorphology in the …

Mesozoic and Cenozoic strata of the San Jacinto Fold Belt (Colombian Caribbean) provide
insights about sedimentary environments and paleogeographic evolution in the transition …

Abstract The Northern Andes in Colombia developed along an active, convergent margin
with a complex subduction-accretion/collision history since Triassic times. Sedimentary …

Linking the long-term with the short-term exhumation history of a mountain range is vital for
understanding the evolution of orogenic topography. Further, erosion rates could be …

The incision of kilometer-scale canyons into high-standing topography is often used to
constrain the surface uplift history of mountain ranges, controlled by tectonic and …