Cone shaped mounds located in Zimbabwe.
- Macrotermes sp.
- 17° 40' 5" S, 27° 52' 14" E
- Köppen Class
On average, 730mm of rain fall here each year, with 519mm (or 71.1%) of that falling during this locations' wettest quarter.
Local SoilThe local soils are primarily lixisols.
|Location||Sand [%]||Silt [%]||Clay [%]|
Joseph, G. S., Seymour, C. L., Cumming, G. S., Cumming, D. H. M., Mahlangu, Z., and Bartha, S. (2013). "Termite mounds as islands: woody plant assemblages relative to termitarium size and soil properties." Journal of Vegetation Science, 24(4), 702-711.
ISRIC – World Soil Information, 2013. Soil property maps of Africa at 1 km. Available for download at www.isric.org.
Hijmans, R.J., S.E. Cameron, J.L. Parra, P.G. Jones and A. Jarvis, 2005. Very high resolution interpolated climate surfaces for global land areas. International Journal of Climatology 25: 1965-1978.
Peel MC, Finlayson BL & McMahon TA (2007), Updated world map of the Köppen-Geiger climate classification, Hydrol. Earth Syst. Sci., 11, 1633-1644.