Figure 1.
![Location of the research area (A); the studied gullies superimposed on a background of the Vilnia valley (B); gully catchments and the main relief forms (C); and the location of drillings on the gully fans (D)Source: Geoportal.lt [29 October 2023]](https://sciendo-parsed.s3.eu-central-1.amazonaws.com/64724862215d2f6c89dc2e1e/j_mgrsd-2023-0026_fig_001.jpg?X-Amz-Algorithm=AWS4-HMAC-SHA256&X-Amz-Content-Sha256=UNSIGNED-PAYLOAD&X-Amz-Credential=AKIA6AP2G7AKOUXAVR44%2F20251205%2Feu-central-1%2Fs3%2Faws4_request&X-Amz-Date=20251205T003803Z&X-Amz-Expires=3600&X-Amz-Signature=196ab9e6831f14bd392ee45450874007f9c6bf35412cb75b9be549eaa0a59fa7&X-Amz-SignedHeaders=host&x-amz-checksum-mode=ENABLED&x-id=GetObject)
Figure 2.
![Longitudinal and cross-sectional profiles of the studied gullies (dashed line - cutting of the fan after building a culvert under the road); m asl - meters above sea levelSource: Geopoprtal.lt [29 October 2023]](https://sciendo-parsed.s3.eu-central-1.amazonaws.com/64724862215d2f6c89dc2e1e/j_mgrsd-2023-0026_fig_002.jpg?X-Amz-Algorithm=AWS4-HMAC-SHA256&X-Amz-Content-Sha256=UNSIGNED-PAYLOAD&X-Amz-Credential=AKIA6AP2G7AKOUXAVR44%2F20251205%2Feu-central-1%2Fs3%2Faws4_request&X-Amz-Date=20251205T003803Z&X-Amz-Expires=3600&X-Amz-Signature=18d6ac4d1d00cc92bcdb6b85a757d420cdd3382553332af874f0607587083598&X-Amz-SignedHeaders=host&x-amz-checksum-mode=ENABLED&x-id=GetObject)
Figure 3.

Figure 4.

Radiocarbon age of the studied fans at the mouth of the gullies (conventional dating), calibrated OxCal v_ 4_4_4 (Reimer et al_ 2020; Bronk Ramsey 2021)
| Lab. index | Sample, no. /depth [m] | Material | 14C age, years (BP) and error, (±1σ) | Calibrated age (cal. AD) for 95.45% probability |
|---|---|---|---|---|
| Vs-2735 | Belmonto 3/1.45 | soil | 1125±200 | 567–1274 |
| Vs-2736 | Belmonto 6/1.40 | peat | 360±70 | 1420–1659 |
| Vs-2737 | Belmonto 7/0.72 | peat | 620±75 | 1271–1435 |
| Vs-2738 | Belmonto 8/0.85 | peat | 1390±70 | 540–777 |