<?xml version='1.0' encoding='UTF-8'?><metadata xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcterms="http://purl.org/dc/terms/" xmlns="http://dublincore.org/documents/dcmi-terms/"><dcterms:title>Field measurements of hydraulic conductivity and soil shear strength at Gabilan Mesa, CA</dcterms:title><dcterms:identifier>https://doi.org/10.7910/DVN/VSRHQU</dcterms:identifier><dcterms:creator>Richardson, Paul</dcterms:creator><dcterms:publisher>Harvard Dataverse</dcterms:publisher><dcterms:issued>2020-03-07</dcterms:issued><dcterms:modified>2020-03-07T13:21:36Z</dcterms:modified><dcterms:description>This data was collected to determine if aspect-dependent differences in field-saturated hydraulic conductivity and soil shear strength exist at Gabilan Mesa, CA. Infiltration and soil shear strength measurements were made at two field locations at Gabilan Mesa on north-facing and south-facing slopes. At each field location, multiple infiltration and soil shear strength measurements were made on north-facing and south-facing slopes. The infiltration measurements were used to estimate field-saturated hydraulic conductivity which is reported here. We also report soil shear strength values made for bare soil and vegetated soil.</dcterms:description><dcterms:subject>Earth and Environmental Sciences</dcterms:subject><dcterms:subject>Geomorphology, hillslope, hydrology, soil strength, hydraulic conductivity, topographic asymmetry</dcterms:subject><dcterms:date>2020-03-07</dcterms:date><dcterms:contributor>Richardson, Paul</dcterms:contributor><dcterms:dateSubmitted>2020-03-07</dcterms:dateSubmitted><dcterms:license>CC0 1.0</dcterms:license></metadata>