LANDFORM IDENTIFICATION TABLE
No Landform Imagery Landform Coordinate Process Information
1 Fault 35° 7'25.76"N
119°39'54.57"W
Structural A fault is a split between two pieces of rock that happens when they slide over each other. This movement can happen because the rock absorbs and stores the tectonic pressure sent by the movement of lithospheric plates. Over time, this pressure builds up until the stress force is strong enough to move the rock along the fault line.
2 Fold 3° 3'31.43"S
102°15'22.50"E Structural Folding is a change in the shape of rock layers caused by force and stress. The rock moves out of its original position to make an arch. Folds happen when pressure is put on the earth's surface in a straight line.
Where the pressure comes from is a process called tectonics, which is caused by forces inside the earth in the form of convection currents that always move in cycles.
3 Horst 7°55'26.57"S
110°29'0.52"E
Structural Graben are plateaus that are sloping downward as a result of the action of endogenous energy.
4 Graben 7°47'36.02"S
110°19'7.35"E Structural Horsts are defined as plateaus that go on to experience a rise as a result of endogenous energy.
5 Parasiter
Cones 21°15'42.58"S
55°43'4.20"E Volcanic parasitic cones that can be found in the foot of the volcano. parasite cones have conical forms. magma extrusion from other branches can be responsible for the formation of parasite cones.
6 Caldera 8°14'48.70"S
117°59'19.22"E Volcanic Explosive eruptions caused the mare land to sink and create the caldera, which is where the caldera was formed. There are four different types of calderas:
destruction, collapse, erosion, and resurgent calderas.
7 Volcanic Cone
8°20'33.11"S 115°30'25.62"E
Volcanic Volcanic cones (kerucut api) are the uppermost portions of a volcano that are in direct contact with eruptive material from below the earth's surface.
8 Crater 8°24'29.93"S
116°24'15.78"E Volcanic One of the volcano's components, the crater is found near the volcano's very tip. Craters are openings where substances such as lava can be released. the crater's size.
can identify the type of eruption and the type of volcano.
9 Riverbar 0°25'32.08"S
116°59'52.75"E Fluvial A riverbar is an area that experiences aggradation as a result of the deposition of sediment carried by the flow of water. Riverbank is found in parts of the river where the flow is slow. The river sandbar is usually spread over the river bed. The river sandbar is divided into three Central Sandbars (often referred to as branching sandbars, found in the woven river type), Edge sandbars.
10 Delta 0°41'47.99"S
117°25'40.61"E Fluvial Detta form as rivers empty their water and sediment in to another body of water.
Delta formed due to deposition sediment carried by river flows
11 Meander 0°21'14.35"S
116°10'11.65"E
Fluvial Meander is a meandering river that is S-shaped.
Meanders occur due to sideways movement due to river currents on formation and changes river curves.
Hamp or most rivers that are straight, there will be twisting currents
and there will be local-local deposits which then in their development can form meanders.
12 Oxbow
Lake
0° 8'55.33"N 101°19'28.69"E
Fluvial Oxbow lake is a bend that can be close to each other and then disconnected from the main channel and becomes a lake. Oxbow Lake occurs due to a very intensive erosion process on the cliff slope. Oxbow is often opened by the community for such and also activities of daily life
13 Sea Stack 8°37'16.23"S 115° 5'12.41"E
Marine sea stack area large stack that looks like a tall stone tower seperated from the main shore, sea stack formed aut to erosion or the slow weathering process
14 Sand Bar 8°45'45.29"S
115°10'9.48"E Marine Gisik or sand bar is a landform characterized by sedimentary material in the form of sand or gravel.
Gisik is also utilized by humans as a place to moor boats for fishermen, the fishing industry, tourism, and residential structures surrounding Gisik land.
15 Cliff 8° 8'47.99"S
110°35'24.81"E Marine
Cliff are a nigh area of rock with a very steep side. Cliff formed due to erotion and weathering process
16 Lagoon 9°29'27.99"S
118°57'35.67"E Marine Laguna or lagoon are an
area of relative
smallow,quier water, and having access to the sea but seperated by barriers.
Lagoon formed when an island completty subsides beneath the water surface and leaving a ring of coral continue
10 grow
17 Karst Hill 8° 8'0.10"S
110°34'0.00"E Karst Karst hill have the enaracteristic of having various shapes such as cones rounds, towers, table, erc.
18 Logva 8° 7'47.12"S
110°34'6.28"E Karst logva are a earst lake that formed due to doline or vvala joint base is covered by impermeable material
due to material
sedimentation
19 Karst Cave 8° 1'43.15"S 110°38'17.85"E
Karst Karst Cave is a room that
located underground and can be acsess by humans.
and has depth of hunderd meters
20 Karst
Tower 20°56'6.57"N
107°10'17.69"E Karst tower karst are is a left over hill From dissolution and erotion. Tower Karst have a tower form and have Steep slope, Karst tower are seperated from each other and surrounded by aluvial plains
21 Longitudin
al dunes 25°26'18.84"N
26°46'32.50"E Aeolian longitudinal dunes or linear dunes have a linear ridges that long 120-200 km. this longitudinal sand dunes formed due to strong winds from two diretion.
22 Barchan
dunes 8° 0'51.19"S
110°18'59.93"E Aeolian Barchan sand dunes is a dunes that have cresent shape. Barchah has a steep slip face whore tips point away from the wind.
Barchan dung can be formed when there is limited Portion of the sand.
23 Star Dunes 30°59'36.93"N
1°43'28.18"W Aeolian star sand dunes are dunes that have a shape like pyramid. that pyramid shapes formed due to multidirectional Wind: Star dunes have three or more ridges that radiates from the center
24 Parabolic
dunes 24°52'52.40"N
51°31'56.45"E Aeolian Parabolic Dunes is a sand dunes that have U-shapes.
most parabolic Sand dunes form near sear
25 Port 6°56'57.46"S
110°25'42.40"E
Anthropogenic An area where ships and boats can dock, load and unload cargo, and offer other services connected to maritime transportation is referred to as a port. Ports play a significant role in aiding trade and the transfer of commodities and are often located around coastlines or navigable rivers.
26 Airport 6° 7'35.19"S 106°39'17.61"E
Anthropogenic A place where planes take off and land is called an airport. It acts as a hub for air travel, with space for passenger trips, cargo shipments, and other services related to flying.
Airports usually have terminals, runways, control buildings, and places for customs, security, and passenger amenities.
27 Resevoir 6°32'14.38"S
107°20'32.79"E Anthropogenic A reservoir is a man-made or natural body of water that holds water and gives it out for different uses. Most reservoirs are made by building dams across rivers or valleys. This makes it possible to collect and keep water. They are important sources of water for irrigation, drinking water, hydroelectric power generation, and tourism.
28 Reclaimed
Beach 6° 5'18.89"S
106°44'46.03"E Anthropogenic A "reclaimed beach" is an area of beach that has been fixed up or made by humans. Land restoration is often used in this process.
This is the process of getting land back from the sea or other bodies of water.
Reclaimed beaches can give people more room to play, help protect the coast, and help with tourism and waterfront development projects.
