The absence of crustal magnetic fields above the martian basins Hellas, Argyre, and Isidis is
often interpreted as proof of an early, before 4.1 billion years (Ga) ago, or late, after 3.9 Ga …

A subset of the sinuous ridges (SRs) in the Aeolis/Zephyria Plana (AZP) region of Mars has
been previously hypothesized to be inverted fluvial features, although the precise induration …

Abstract The Walker Lane belt of eastern California and western Nevada is the northernmost
extension of the Gulf of California transtensional rift, where the process of continental rupture …

The Sierra Nevada of California is the longest and tallest mountain range in the co-terminus
USA, and has long been regarded as topographically very young (< 6 Ma); however, recent …

Abstract The Middle to Late Miocene Bodie Hills volcanic field is a> 700 km2, long-lived (∼
9 Ma) but episodic eruptive center in the southern segment of the ancestral Cascades arc …

Ongoing arc magmatism along western North America was preceded by ancestral arc
magmatism that began ca. 45 Ma and evolved into modern arc volcanism. The southern …

Abstract The Walker Lane currently accommodates∼ 20% of the dextral motion between the
Pacific and North American plates. This accommodation occurs on regional-scale systems of …

Magmatism is an important driver of landscape adjustment over∼ 10% of Earth's land
surface, producing 103‐to 106‐km2 terrains that often persistently resurface with magma for …

The geometry and dimensions of sedimentary basins within the Walker Lane are a result of
Plio‐Pleistocene transtensive deformation and partial detachment of the Sierra Nevada …

We integrate new geochronological, petrographic, and geochemical data with previously
published (Sierra Crest–Little Walker volcanic center) and new (Ebbetts Pass volcanic …