Remontides

Remontides is a term that does not have a single, widely accepted definition in established disciplines. The word appears as a neologism in scattered sources, often drawing on the French remontée, meaning an upward movement or resurgence. Because there is no consensus on its meaning, remontides is best treated as a provisional label rather than a formal scientific category.

In coastal geomorphology, some authors have used remontides to describe episodic shoreline or riverbed changes that occur through cycles of erosion and deposition influenced by tides and local uplift. In these uses, the term is meant to capture short-term or intermediate-scale adjustments rather than long-term transgressions or regressions. However, this application is not standardized, and different authors may attach different specifics to the concept.

In hydrological or karst contexts, remontides has occasionally appeared in regional reports or theses to denote transient groundwater upwellings or surface expressions of subsurface hydrological processes. Again, the term lacks a uniform definition, and its interpretation can vary depending on the study or author.

Because remontides lacks a stable, agreed-upon meaning, it is most often encountered in exploratory or speculative writing rather than in entry-level or mainstream scientific literature. If you encounter the term in a particular publication, the intended meaning is likely defined by that author. As of now, there are no established, universally recognized definitions or standards for remontides.