Safdarjung’s Tomb | New Delhi

Information

Landmark: Safdarjung’s Tomb
City: New Delhi
Country: India
Continent: Asia

Safdarjung’s Tomb, New Delhi, India, Asia

Bukit Bang Taong is a geological formation located in the Tutong District of Brunei.

Visual Characteristics

The formation consists of sedimentary rock outcrops with exposed layers. Vegetation is moderate, primarily consisting of low-lying shrubs and grasses adapted to the exposed conditions. The rock surfaces exhibit weathering patterns, including erosion channels and lichen growth.

Location & Access Logistics

Bukit Bang Taong is situated approximately 15 kilometers inland from the Tutong town center. Access is via Jalan Bukit Udal, a paved road. A short, unpaved track branches off Jalan Bukit Udal, leading to a small parking area at the base of the formation. No public transport services operate directly to this location.

Historical & Ecological Origin

The geological origin of Bukit Bang Taong is attributed to sedimentary deposition during the Miocene epoch. The exposed rock layers provide evidence of ancient marine environments. Ecologically, it represents a transition zone between lowland forest and more exposed, scrubland habitats.

Key Highlights & Activities

Observation of geological strata is possible. Short walks on the established paths around the base are available. Photography of the rock formations and surrounding landscape can be undertaken.

Infrastructure & Amenities

There are no dedicated facilities at Bukit Bang Taong. Restrooms, shade structures, and food vendors are not present. Cell phone signal (4G/5G) is intermittent and generally weak.

Best Time to Visit

The optimal time for photography is during the early morning or late afternoon when the sun angle provides defined shadows on the rock faces. The dry season, from March to September, offers the most favorable weather conditions with reduced rainfall.

Facts & Legends

Local folklore suggests that the distinct layering of the rocks at Bukit Bang Taong represents the petrified folds of a giant serpent that once guarded the area. Geologists, however, attribute these formations to tectonic uplift and erosion.