1. External geological agents such as wind, glaciers, water and sea water can cause erosion and sedimentation processes that shape the Earth's surface over time. Wind forms desert pavements and mushroom rocks through deflation and abrasion, and causes aeolian sedimentation forming dune types like barchan and star dunes. Glaciers erode and transport material, forming landforms like moraines. 2. Water agents like rivers and streams erode through processes like mass wasting. Rivers progress through stages from youth to maturity that change their valleys and floodplains. Groundwater is stored in aquifers and can dissolve carbonate rock to form karst landscapes with sinkholes and caves.

1. External Geological Agents
1. WIND: can cause erosion, mass wasting and sedimentation
 The main erosion processes cause by wind are:
DEFLATION forms a layer of rocks that is called a desert
pavement (stony field - reg).
ABRASION forms mushroom-shaped rocks

2.  Aeolic sedimentation when wind finds an obstacle in the landscape
Sand dunes are formed (in sandy deserts (ergs))
Differents types of dunes: Barchan dunes
Star dunes
Transverse dunes

3. 2. GLACIERS: are divided into an accumulation zone and an ablation (wastage)
zone along an equilibrium line. Glaciers are made up ice and snow, water, rocks
and sediments. A glacier moves very slowly (few centimeters to a few meters
each day).

4. • There are different types of glaciers:
Alpine glaciers: cirques, horns, arete , U-valley, moraines (lateral, medial,
end)

5. Continental glaciers: which are continuous masses of ice that are much larger than
alpine glaciers. Small continental glaciers are called ice fields. Big continental glaciers
are called ice sheets.

6. 3. Wild water:
GREAT AMOUNT OF
WATER
STREAMS
STREAMS ARE NON DEFINED NOR
PERMANENT COURSES OF WATER
RAINSTORM MODIFY THE RELIEF
Smooth and
homogeneous
SOIL
easily eroded
Heterogeneous
SOIL
some parts are
harder to erode
FAIRIES’
CHIMNEYS
RILL
GULLY
TORRENTS
 Intermittent , short
water courses
 very steep slopes
fixed channel
ice melts or a period
of heavy rains.

7. • 4. RIVERS:
• 0.0001% of the Earth's water .
• Different sources: lakes , springs (from underground), rain or melting snow
and ice (high mountains)
To narrow river consider its drainage basin and its floodplain:
drainage basin flood plain

8. Rivers (masswasting processes)

9. 1.Early maturity V-shape
valley
2. Late maturity.
Flat-floored
valley .
Narrow flood
plain. River begins
to meander. Flood
plain widens
3. Old age. Very
wide flood
plain. Cut-off
meanders (ox-
bow lakes)
Rivers (erosion) three valley shape.

10. • 5. Ground water
• Groundwater : water in the ground is stored in the spaces between rock particles.
• A groundwater aquifer is an underground layer that holds water within soil,
porous rock, or similar material.
• A groundwater well may be used to extract water from a groundwater aquifer.

11. • Karst relieves are landscapes shaped by the dissolution of a soluble bedrock layer,
(usually carbonate rock such as limestone or dolomite) by a mildly acidic water.
• These landscapes display different:
• surface landforms (sinkholes, dolines, disappearing and reappearing streams,
poljes)
• underground features (extensive caves and cavern systems may be formed. In
caves, the deposition of calicium carbonate may form stalactites, stalagmites,
column)

13. SEA WATER
waves, tides,
sea currents
erosion, transport,
sedimentation
processes
is constantly moving
has a lot of energy
•6. Sea water in coastal areas
THEY MODEL
COASTAL AREAS
WAVES
Chemical
Physical
weathering
Erosion
Salty sea reacts in
chemical ways with
rocks and makes
them weaker
Stones, other sediments
are carried by waves
and they crash into
the coastal rocks.
Cliffs,
sea caves, arches,
abrasion platforms,
sea stacks
LANDFORMS

16. WAVES
Transport and
sedimentation of
materials
Beach: deposition of
sand and gravel along
the shoreline
Longshore drift:
This process is when individual particles are moved along the beach in a zig-
zag pattern

17. Longshore drift Spits, bay barrier, barrier island, tombolos, lagoons…
LANFORMS

18. The sediments (sand, mud
and pebbles)
accumulate in sedimentary
basins , forming layers or
plies.
These layers of sediment are sinking
deeper and deeper into the basins.
Under conditions of
high temperatures
and
high pressures
The sediments become rock
(lithified) through a process called
DIAGENESIS (it may take millions
of years)
SEDIMENTARY ROCKS
Clastic sedimentary rocks such
as conglomerate, sandstones,
shale .
Chemical sedimentary rocks,
such us halite, gypsum
Organic sedimentary
rocks such us limestone, coal.
Types of sedimentary rocks

19. CONGLOMERATE SANDSTONE SHALE
HALITE
COAL
LIMESTONE
GYPSUM