In an effort to understand sources of nitrate (NO-3) in surface waters of high-elevation catchments, nitrogen (N) transformations in and under seasonal snow were investigated from 1993 to 1995 on Niwot Ridge, an alpine ecosystem at 3,500 m located in the Colorado Front Range of the Rocky Mountains. Ammonium (NH+4) and NO-3 labeled with 15N applied as nonconservative tracers to the snow showed no evidence of nitrification in the snowpack. Furthermore, NH+4 movement through the amended snowpack was highly correlated with a conservative chloride tracer (r2=0.99). In an unamended snowpack NH+4 concentrations in meltwater before contact with the ground were highly correlated with NO-3 concentrations (r2=0.98), which is consistent with no nitrification in the snowpack. The isotopically labeled 15NH+4 applied to the snowpack was found in underlying soils, showing that NH+4 released from snow can be rapidly immobilized. Resin bag (mixed-bed ion-exchange resins) measurements (n=22) showed that 80% of the mobile inorganic N in unamended subnivial soils was NO-3. Measurements of KCl-extractable inorganic N from surface soils showed that highest values were prior to the initiation of snowmelt and lowest values were during the growing season. The natural Δ15N abundance of unamended soils was negative and ranged from -12 to -2, suggesting that atmospheric deposition of Δ15N-depleted N is an important component of N cycling in these alpine soils. These results suggest that soil mineralization under seasonal snow, rather than snowmelt release of NO-3, may control NO-3 concentrations in surface waters of high-elevation catchments. ¿ American Geophysical Union 1996