Geoscience Reference
In-Depth Information
Mambova
Mambova
Rapids
Mambova
Rapids
22°
24°
26°
26°
Rapids
L.
Kariba
Katombora
Katombora
Rapids
Katombora
Rapids
18°
18°
a
Victoria
Victoria
Falls
Victoria
Falls
Rapids
Falls
Goha
Hills
S
S
Sh
Hwange
a
Ts
Seronga
Seronga
sa
sa
S
S
Sp
Mababe
i
i
a
o
a
a
G
G
R
R
N
a
a
Aha
Hills
e
e
Stream cut
scarp
20°
20°
20°
Tsau
Drotsky's
Drotsky's
Caves
Drotsky's
Caves
Tsau
i
Caves
Toteng
Toteng
b
b
Makgadikgadi
b
b
Khwebe
Khwebe
Hills
Khwebe
Hills
b
Ngami
Hills
f
f
Simoane
River
Ntwetwe
Ntwetwe
Pan
Ntwetwe
Pan
Haina
Haina
Hills
Haina
Hills
Hills
Pan
Sua
Pan
L.
Dow
L.
Dow
L.
b
b
Dow
Francistown
GHANZI
e
e
KEY
S
Sh
Sehitwa
Shakawe
22°
Sp
Sepopa
Gomare
Nokaneng
Rakuku
Tsodilo Hills
Kunyere River
Mokhakhelo River
Alab dunes
1.7 km apart
Longitudinal dunes
200m apart
Sand ridges
Transverse ridges
50m apart
Transverse
hummocky dunes
Linked barchans
Faint furrow
patterns
g
g
G
Kuli
N
g
g
R
Ts
K.
M.
Letlhakeng
Letlhakeng
24°
24°
TSANE
a
Kakong
Sekoma
MOLEPOLOLE
MOLEPOLOLE
b
c
d
d
d
e
Water's En d
f
Pitshane
Pepani Laagt e
MAFIKENG
Tshabong
26°
g
Rock outcrops in
the Ghanzi area
Low islands in
Okavango Swamp
0
100 km
c
c
Khuis
Khuis
0
100 mls
22°
24°
26°
Figure 4.1
Landform diversity in the Kalahari Desert. Originally mapped from air photographs by Grove (1969), subsequent
analysis in the field has demonstrated how Quaternary climate change has played a significant role in shaping the depositional
