霜降Frost's Descent
大坑口
Dàkēngkǒu

Dakengkou

sourced
iddakengkou
dakengkou

East–west canyon carrying the Da Hong Pao road from the Chongyang side up to Tianxin; the main stream of the Jiulongke–Daoshuikeng–Tianxin area. Counted as a 'pit' only in some lists.

Level
Sub-area
Within
Fujian › Nanping › Wuyishan › Wuyi Mountain Scenic Area
Terroir class
Zhengyan 正岩 · "true rock", core scenic area

Where it lies#

Tea places nearby, plotted by their coordinates. Only physical positions are shown, no boundaries.

NanpingWuyishan › Wuyi Mountain Scenic Area · Parent region shown
Nearby tea placesWuyi Mountain Scenic Area · Parent region shown

Terroir#

Soil
Deep, nutrient-rich, with silt carried down the stream.
Slope and light
Both sides of an east–west canyon (east- and west-facing slopes), forest- and ridge-shaded; abundant water.

Local words#

Other names and written forms 1#

Romanisations
  • Da Keng Kou

Names and ambiguities#

Is Dakengkou one of the 'three pits'?

The usual list of the three pits is Niulankeng, Huiyuankeng and Daoshuikeng. Some Chinese commercial articles add Dakengkou as well, giving four 'pits' under the same slogan. Forum sources describe Dakengkou as a canyon road toward Tianxin Rock rather than a core pit.

14

Notes#

Community sources describe Dakengkou as an east–west canyon that links the Tianxin water system with the Chongyang River, with the Da Hong Pao scenic road along it and a Maitreya statue at its mouth; Tianxin Yongle Temple lies on the same line. It carries the main stream draining Jiulongke, Daoshuikeng and Tianxin, so water is plentiful and soils are deep and fertile with silt brought down from above. Tea grows on both sides, on east- and west-facing slopes, shaded by forest and ridges. Its deeper, richer soils set it apart from the narrow rock pits. Jing Tea Shop counts Dakengkou as one of the three pits (instead of Daoshuikeng).

Sources#

  1. Reporting and journalismaccessed 2026-10-18

    Partly promotional. Its Qidan genetics claim is attributed to Fujian Agriculture and Forestry University; the underlying paper is not identified here.