DigitalCommons@USU
metadata only
Terminal Miocene Arrival of Colorado River Sand in the Salton Trough, Southern California: Implications for Initiation of the Lower Colorado River Drainage
Two competing hypotheses have been proposed for initiation of the lower Colorado River (CR): upward-migrating headward erosion (predicts gradual expansion of catchments), or downward-propagating lake-overflow events (predicts rapid insertion of river discharge into the lowland region). New data from
Conceptio Open Archive
Analyze & explore related research in Conceptio
Connect this record directly into your research workflow or AI agent. Explore citations across open repositories, query full text, and export structured proof bundles.
This document is indexed with metadata only: full text is not available in the archive for this record. Open the official source ↗
Related documents
- Late tertiary synorogenic sedimentation in the northern Livermore Basin, California#488703
- Preliminary geologic map of the Goat Mountain quadrangle, Albany and Laramie counties, Wyoming.#627364
- Decoupling Taxon Completeness and Phylogenetic Instability in Macronarian Sauropod Morphological Datasets#1054930
- Miocene to present turnover of molluscan assemblages: insights into coastal-marine ecosystem evolution along the Peruvian Margin#121807
- A new class of monthly rainfall-runoff models for ungauged basins - Application to the Peruvian coastal basins#254315
Record · ID 1165401
Retrieved via Conceptio: every document is proof-bundled with source, license, and retrieval metadata.
Retrieved via Conceptio: every document is proof-bundled with source, license, and retrieval metadata.
Bring this data into your agent: Connect via MCP or API · 20 free credits to start · no card required
Read the Docs → · View CLI source on GitHub · Conceptio Open Knowledge Archive
Read the Docs → · View CLI source on GitHub · Conceptio Open Knowledge Archive