Northwest Africa 13683 (NWA 13683) Adrar, Algeria Find: 2018 Classification: Rumuruti chondrite (R3-6) History: Found between 2018-2019. Many meteorites weighing a total of 1959 grams were purchased by Adria_n Contreras Gómez from a Sahara seller in July 2020. Physical characteristics: Sample lacks fusion crust, is irregular-shaped and shows abundant chondrules surrounded by sulfides. Petrography: Description and classification (A. Love, App) Sample is a genomict chondrite breccia composed of rounded to angular clasts of unequilibrated and recrystallized textures occurring within a host of slightly flattened, dispersed chondrules, fragments and sulfide grains. Recrystallized clasts lack discernible chondrules and low Ca pyroxene, and contains a network of 50µm secondary plagioclase. Chondrules average apparent diameter 424µm (n=105). Additional minerals are: troilite, abundant pentlandite, phosphate and chromite. Geochemistry: Host: olivine (Fa32.2±14.3, CV%=43 (R3.5), Fe/Mn=80.7±23.0, n=30); low Ca pyroxene (Fs6.6±6.0Wo1.0±0.8, Fe/Mn=19.7±11.6, n=7); pigeonite (Fs21.4±2.9Wo9.5±2.7, n=3); unequilibrated clast: olivine (Fa20.1±14.4, CV%=72 (R3.2), Fe/Mn=62.6±30.6, n=12); recrystallized clast: olivine (Fa37.6±0.1, Fe/Mn=73.1±3.6, n=6); high Ca pyroxene (Fs13.4±0.1Wo39.1±0.4, Fe/Mn=36.8±2.2, n=3). Classification: Rumuruti chondrite (R3-6, C-S2, wi-2) Chondrule diameter, magnetic susceptibility, ubiquitous pentlandite and lack of FeNi metal suggest sample is an R chondrite. Based on unequilibrated compositions and coefficient of variation w/in clast and host, sample is an R3.2-6. The original CoA is also included.