The Neuné rises within the commune of Gerbépal in the parc naturel régional des Ballons des Vosges, which also contains a part of its length. It flows first to the north-west, then towards the west, and finally towards the south-west where it joins the right bank of the Vologne, at the level of the small settlement of Champ-le-Duc. The Neuné's principal tributary is the B'Heumey, which joins with it in the commune of Chapelle-Devant-Bruyères.
Le Neuné is a substantial river. Its flow rate has been measured over a 22-year period at Laveline-devant-Bruyères, which is slightly away from its confluence with the Vologne. The drainage surface studied is, or 97 percent of the total watershed of the river. The average interannual flow rate, or discharge of the river at Laveline-devant-Bruyères is. The Neuné exhibits moderate seasonal fluctuations in flow rate. The high-water period occurs in the winter season, with average monthly instantaneous flow rates varying between from November to March inclusive, with an overall maximum in March and a secondary maximum in January. From April onwards, the flow rate drops off quickly and continues until the low-water period, which occurs from July to September, with minimum monthly average instantaneous flow rate going down to in August, still a comfortable flow for a small river. Fluctuations in flow rate can be more significant from year to year and over short time periods. At low water, the three-year low instantaneous flow rate can drop to in the case of a dry five-year period, or about, which is not too severe. As for floods, they can also substantial, considering the relatively small watershed. The Instananeous Maximum Flow Rate over 2 years and the IMFR5 are respectively. The IMFR10 is and the IMFR20 is, while the IMFR50 has not been calculated due to an insufficient history of measurements. The volumes of the Neuné's floods rise to as much as 30 percent of those of the Vologne. The maximum instantaneous flow rate recorded at Laveline-devant-Bruyères during this period was on 30 December 2001, while the maximum daily average flow rate was on 4 October 2006. Comparing the first of these numbers with the different IMFR measurements of the river suggests that this flood was of the order of a 20-year event. The Neuné is a substantial river. The runoff curve number in its watershed is annually, which is over twice the overall average of France with all basins taken together, and clearly greater than the average of the French basin of the Moselle, which is downstream of Metz). The specific flow rate of the river attaches a solid number to this fact: 23.6 litres per second per square kilometre of basin.
