| 0 | NA 89075 | 2024RJLPA-001 | Rhododendron maximum L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/18/2024 | Fieldstone Farm Tank Creek Nature Preserve (a property of the Pocono Heritage Land Trust): Collected along Tank Creek. The property is accessed from a parking area located on Devil's Hole Road. | 41.13862300, -75.34562700 | 493 | Mostly found in mixed deciduous forest with occasional conifers and evergreen shrubs generally on steep slopes above Tank Creek in rocky well-drained soils in shade to part-shade. The slopes are abundant in decomposed organic matter and runoff soils. Slope: 5 to 30 percent. Aspect: various. Geology: The underlying geology of this area is of Devonian origin and characterized as the Long Run Member of Catskill Formation. It is comprised of gray and grayish-red sandstone and grayish-red siltstone and mudstone in fining-upward cycles. (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type found here is classified as Alluvial Land. In geology, alluvial land refers to areas of land that are formed by the deposition of sediments carried by rivers, or other surface water. EPA Ecoregion (Level III): North Central Appalachians (62). EPA Ecoregion (Level IV): Low Poconos (62b). | Wild material | | 2169039 | NA 89075 |
| 1 | WLP 1705 | NA 83948 | Rhododendron maximum L. | Kentucky, United States | NA | | | 2016 | COLLECTED | 09/29/2016 | Kentenia State Forest, Pine Mountain, on Route 1679, north side. | 36.91400000, -83.25900000 | 758 | Roadside. | | | 1950864 | WLP 1705 |
| 2 | NA 89070 | AFGN25-16 | Rubus odoratus L. | North Carolina, United States | NA | | | 2025 | COLLECTED | 06/03/2025 | Ball Creek Rd (83). | 35.03127000, -83.45786000 | 1334 | Mixed mesophytic Appalachian forest. | Wild material | | 2191433 | NA 89070 |
| 3 | NA 89076 | 2024RJLPA-002 | Kalmia latifolia L. | Pennsylvania, United States | NA | | | 2024 | COLLECTED | 09/18/2024 | Fieldstone Farm Tank Creek Nature Preserve (a property of the Pocono Heritage Land Trust): Collected along Tank Creek. The property is accessed from a parking area located on Devil's Hole Road. | 41.13862300, -75.34562700 | 493 | Mostly found in mixed deciduous forest with occasional conifers and evergreen shrubs generally on sloping sites as an understory shrub in rocky well-drained soils in shade to part-shade. Slope: 5 to 15 percent. Aspect: various. Geology: The underlying geology of this area is of Devonian origin and characterized as the Long Run Member of Catskill Formation. It is comprised of gray and grayish-red sandstone and grayish-red siltstone and mudstone in fining-upward cycles. (Source: USGS Pennsylvania Geologic Map Data). Soils: The primary soil type found here is classified as Alluvial Land. In geology, alluvial land refers to areas of land that are formed by the deposition of sediments carried by rivers, or other surface water. EPA Ecoregion (Level III): North Central Appalachians (62). EPA Ecoregion (Level IV): Low Poconos (62b). | Wild material | | 2169040 | NA 89076 |
| 4 | WLP 3435 | RM2023-004 | Aristolochia macrophylla Lam. | North Carolina, United States | NA | | | 2024 | COLLECTED | 10/20/2023 | Plants growing on slopes above Big Creek Road on a trail up from cabins toward the Appalachian Trail. | 35.00179600, -83.45508900 | 752 | Plants growing along a rocky stream in part shade. Slope: 25 percent. Aspect: Variable. The underlying geology of this area is Coweeta Group, primarily of Late Proterozoic origin. It is comprised of quartz dioritic gneiss, feldspar-quartz-biotite gneiss, metasandstone and quartzite, alumino-silicate schist, garnetiferous biotite gneiss, and minor amphibolite. Quartz dioritic gneiss is predominant. (Source: USGS North Carolina Geologic Map Data.) The primary soil type in the collection area is classified as Cullasaja-Tuckasegee complex, 15 to 30 percent slopes, stony. The Cullasaja series consists of very deep, well drained soils on benches, toe slopes, foot slopes, drainageways, and fans in coves in the Southern Blue Ridge mountains. They formed in colluvium derived from materials weathered from felsic to mafic high-grade metamorphic and igneous rocks such as granite, mica gneiss, hornblende gneiss, and schist. Slope ranges from 8 to 95 percent. The Tuckasegee series consists of very deep, well drained soils on gently sloping to very steep benches, foot slopes, toe slopes, drainageways, and fans in coves in the Southern Blue Ridge mountains. These soils formed in colluvium derived from materials weathered from igneous and high-grade metamorphic rocks such as granite, mica gneiss, hornblende gneiss, and schist. Slopes range from 2 to 95 percent. (Source: NRCS Web Soil Survey.) | Wild material | | 2166144 | WLP 3435 |