Groundwater contamination in a fractured rock aquifer is very difficult to remediate. An understanding of the transport mechanisms that occur in the fractures and the rock matrix is important in order to implement cleanup strategies such as in situ bioremediation. The Snake River Plain aquifer underlying the Test Area North site at the Idaho National Engineering and Environmental Laboratory is hosted in fractured basalt and is contaminated with trichloroethylene, its degradation products, and other compounds. The objective of this study was to examine and compare responses of various tracers to gain an understanding of transport characteristics in the aquifer and assist in the cleanup of the TAN site.A multiple-well, recirculating, radially convergent tracer test was conducted at the University of Idaho Ground Water Research site, on Columbia River basalt, in Moscow, Idaho. The test focused on a horizontal fracture zone (E fracture) formed as the result of cooling lava. Conservative or near-conservative tracers and particulate tracers included fluorescein, iodide, veratryl alcohol (VA), polystyrene noncarboxylated fluorescent microbeads (6 lm) and Bacillus thermoruber spores. The tracer test results indicate that transport is governed by preferential pathways and is affected by aquifer heterogeneity, advection, dispersion, molecular diffusion, channeling, transport in different channels, and borehole storage. In this short duration experiment, transport was not significantly affected by sorption or matrix diffusion. The particulate tracers may also be affected by density and filtration, as seen by the very low tracer recovery.There are many implications from the outcome of this tracer test regarding the use of various tracers. Fluorescein and VA exhibited a breakthrough curve similar to iodide, and consequently are considered conservative tracers in this environment. The early arrival of polystyrene particle tracer relative to dissolved tracers provides an insight into the preferential flow paths of the system. Bacillus thermoruber spores were not found in any of the wells used in the test; this could be due to filtration, sorption, density affects, predation, or the result of laboratory analysis problems. Without further testing, these spores are not recommended as groundwater tracers.