Japan Geoscience Union Meeting 2024

Presentation information

[E] Poster

H (Human Geosciences ) » H-TT Technology & Techniques

[H-TT15] Geographic Information Systems and Cartography

Wed. May 29, 2024 5:15 PM - 6:45 PM Poster Hall (Exhibition Hall 6, Makuhari Messe)

convener:Takashi Oguchi(Center for Spatial Information Science, The University of Tokyo), Yuei-An Liou(National Central University), Ruci Wang(Center for Environmrntal Remote Sensing, Chiba University), Masahiro Tanaka(Graduate School of Arts and Sciences, The University of Tokyo)

5:15 PM - 6:45 PM

[HTT15-P01] Morphological Analysis of Alluvial Fans in Northern Luzon, Philippines

Noelynna Ramos1, *Takashi Oguchi2 (1.National Institute of Geological Sciences, College of Science, University of the Philippines Diliman, 2.Center for Spatial Information Science, The University of Tokyo)

Keywords:alluvial fans, geomorphology, Solsona Basin, Philippines

The Solsona Basin is a low-lying region in northern Luzon that developed from various stages of tectonic deformation along two parallel sinistral faults of the Philippine Fault Zone. East of the basin, Quaternary alluvial fans have been reported with an average slope of about 1.1°. To understand the various factors affecting the formation of alluvial fans in this tectonically active region, we determined their geometry and other morphological characteristics using a 5-m resolution IFSAR DEM and GIS. The morphometric characteristics of source catchments were also derived to explain the underlying controls (e.g., lithology, tectonics, climate) that affect the morphology of alluvial fans in this region.

Several distinct alluvial fans were recognized along the foothills that border the Solsona Basin to the east. The area of alluvial fans (Af) ranges from 4 to more than 50 km2, while the area of source catchments (Ac) ranges from 10 to 150 km2. The initial correlation of Af and Ac values shows a non-linear relationship between the area of an alluvial fan and the area of its source catchment (i.e., fan size does not necessarily increase as the catchment size increases). From DEM-based measurements, the average slope of alluvial fans and their source catchments are 3.5° and 29.8°, respectively. Source catchments with relatively higher average slopes also have more first-order streams and higher stream length total. From the alluvial fan toe to the drainage divide, the average slope of the longitudinal profiles ranges from 4.5° to 7.6°. While still preliminary, these geometric and morphological attributes of alluvial fans and their source catchments provide fundamental information for understanding the various processes that influence the formation and development of these terrestrial deposits in the Solsona Basin. Future work will explore the utility of other morphometric indices and analysis of alluvial fans in other parts of Luzon Island.