Sekumpul Waterfall (Indonesia) – Location, Height, Geography & Facts

Sekumpul Waterfall, Indonesia.

Country: Indonesia
Coordinates: 8.1776° S, 115.1825° E

Sekumpul Waterfall overview

Sekumpul Waterfall is a multi-tiered waterfall in northern Bali, Indonesia. It is significant as a cluster of closely grouped cascades that descend from the island’s highland escarpment, forming a set of distinctive plunge pools and spray zones. The site is notable for its multi-tributary arrangement and for draining upland springs that contribute to the local watershed. Sekumpul Waterfall functions as a measurable geomorphological example of cascade formation on Bali’s volcanic terrain.

Sekumpul Waterfall coordinates

Sekumpul Waterfall is commonly mapped at approximately 8.1776° S, 115.1825° E, or -8.1776, 115.1825 in decimal degrees.

Degrees: 8.1776° S, 115.1825° E

Decimal: -8.1776, 115.1825

Where Sekumpul Waterfall is located

Sekumpul Waterfall is located in Buleleng Regency on the northern side of Bali, Indonesia, on the slopes of the island’s highland zone. The falls sit near the village area known locally as Sekumpul and lie within the hinterland northwest of the coastal town of Singaraja. The waterfall system occupies a ravine fed by upland springs that drain toward the Bali Sea, and it is set against the ridgelines commonly called the Munduk highlands. Steep terraces and narrow gorges surround the cascade cluster.

Why Sekumpul Waterfall is important

Sekumpul Waterfall matters for its concentrated arrangement of separate plunges emerging from adjacent streamlines, a pattern that differs from single-drop waterfalls elsewhere on Bali. The falls supply perennial streamflow to downstream agricultural plots and lowland channels, linking highland recharge areas to local water use. Ecologically, the spray zone and surrounding ravine sustain patches of montane riparian vegetation uncommon on nearby slopes. Geomorphologically, the juxtaposition of layered volcanic bedrock and alluvial deposits creates discrete ledges that produce the waterfall’s multiple drops.

History of Sekumpul Waterfall

The waterfall formed through progressive incision as upland springs and tributary streams eroded volcanic deposits and older lava flows in Bali’s northern highlands. Differential erosion of harder flow-banded lavas and softer pyroclastic layers produced the ledges and steps that now appear as separate cascades. Over human history, surrounding villages have referenced the falls in land boundaries and local resource use, with upland watercourses feeding agriculture below. Changes in upland land use have altered sediment delivery and vegetative cover, influencing the morphology of plunge pools and channel floors adjacent to the waterfall.

Natural features of Sekumpul Waterfall

Sekumpul Waterfall comprises multiple narrow plunges that fall from a single escarpment band into deep, rock-lined plunge pools. The cliff face shows layer-banded volcanic rock interspersed with weathered tuff and colluvial deposits, producing staggered ledges and overhangs. Spray and mist have produced moss- and fern-covered rims, while small talus benches collect coarse sediment below certain drops. Channels dissect the cliff face in parallel lines, creating curtain-like water sheets where springs concentrate along fissures in the bedrock.

Environment, protection, and monitoring of Sekumpul Waterfall

Land containing Sekumpul Waterfall is included in regency-level land-use planning and is subject to customary village governance concerning upland forest and water resources. Conservation themes for the area emphasize watershed protection, erosion control, and maintenance of riparian corridors that support native montane species. Local administrative units and customary authorities coordinate monitoring of land-use change and water quality as part of long-term stewardship, while provincial environmental offices provide broader regulatory oversight for upstream catchment management.

Sekumpul Waterfall facts

Sekumpul Waterfall appears on regional topographic maps that document Bali’s inland watercourses and highland ravines. The cascade system is fed primarily by multiple spring-fed streams that originate in the northern Bali highlands. The name "Sekumpul" is also used in nearby village and land parcel identifiers within local administrative records. The waterfall is visually distinctive for its parallel narrow plunges that descend from a single continuous cliff band. Management of the land around Sekumpul Waterfall is handled through regency-level planning and customary village governance rather than through national park designation.

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