5 -Sediments and Surface Transfers Flashcards

1
Q

Fragmented materials that originate from weathering and erosion of rocks or unconsolidated deposits and are transported by, suspended in, or deposited by water.

A

Sediments

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2
Q

soil material subsequently transported away from its source, mostly by water

A

Sediments

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3
Q

it is essentially the erosional environment (source of sediment)

A

Land

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4
Q

It is essentially the Depositional Environment

A

Sea

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5
Q

Mineral grains (mostly quartz, muscovite), rock fragments and volcanic debris

A

Sandstone

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6
Q

breakdown products, organic debris mainly dominated by plant material

A

Clay

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7
Q

organic debris dominated by marine shell debris, dominantly calcite solutes from sea water due to biological activity

A

Limestone

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8
Q

It is the movement of sediments

A

Sediment transport

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9
Q

How sediments are collected and added to a landform or landmass

A

Sediment Deposition

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10
Q

It is the far most important agent of sediment transport, followed by WIND and ICE

A

Water

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11
Q

when suspended in water, coarser debris have lower velocities than finer debris

A

Stoke’s Law

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12
Q

Water’s ability to transport sediment depends on its ____

A

Velocity

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13
Q

____ works on the steeper slopes producing landslides and colluvium (loose unconsolidated soil in hillsides(

A

Gravity

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14
Q

It moves only fine particles

A

Wind

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15
Q

_____ Transports are powerful, but restricted by climate

A

Ice

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16
Q

_____________ may blast debris over limited distances

A

Volcqnic activity

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17
Q

Sediment deposition that are sorted and stratified, mostly sand and clay. Mostly forms alluvium and lake sediments

A

Water on land

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18
Q

Sediment deposition which is the final destinstion of sediments.

A

Sea

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19
Q

Sediment Deposition which is unsorted debris dumped in the melt zones of glaciers

A

Ice

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20
Q

The process by which a weak, loose sediment is turned into stronger sedimentary rocks

A

Lithification

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21
Q

Lithification is also known as _____ in geology and _____ in engineering

A

Diagenesis , Consolidation

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22
Q

Refers to the changes which take place to the sediments after depositions

A

Lithification

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23
Q

Induced by burial pressure and increased temperature and is characterized by notable strength increase

A

Lithification

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24
Q

The three makn processes of Lithification

A

Compaction
Cementation and
Crystallization

25
It is restructing and change in grain packing, with decrease in volume due to burial pressure, with consequent reduction of porosity as water is squeezed out.
Compaction
26
The filling of the inter-granular pore spaces by deposition of a mineral cement brought in by circulating ground water.
Cementation
27
a small scale of solution and deposition of mineral, so that some grains become smaller and some become larger. This is similar to cementation but the results are stronger than mosaic fixture
Crystallization
28
Formed by weathering processes that break down rocks into pebble, sand or clay particles by exposure to wind, ice, and water (moving fluids) aka DETRITAL ROCKS
Clastic Sedimentary Rocks
29
Formed by chemical reactions and precipitation of different elements dissolved in water chiefly in the ocean aka CHEMICAL ROCKS
Non-clastic sedimentary rocks
30
Example of Clastic rocks (5)
``` Conglomerate Breccia Sandstone Siltstone Shale ```
31
It is composed of rounded gravel, pebbles, cobbles or boulders along with similar rock pieces
Conglomerate
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Similar to conglomerate but its gravel, pebbles, cobbles or boulders have a sharper, angular shape
Breccia
33
Composed of sand
Sandstone
34
Composed of silt
Siltstone
35
Composed of clay-sized particles | smaller than 4 micrometers in diameter
Shale
36
Example of Non-clastic sedimentary rocks (4)
Limestone Halite Rock Gypsum Chert
37
Composed of mineral calcite, may contain or may be made of marine fossils, formed by precipitation from water
Limestone
38
Composed of sodium and chlorine, formed by evaporation
Halite
39
Composed of gypsum, formed by evaporation
Rock Gypsum
40
Composed of microscopic mineral grains of quartz, very hard with sharp edges
Chert
41
Refers to the way sediment layers are staxked kver each other and can occur on the scale of hundreds of meter, and down to submillimetwr scale. It is a fundamental feature of sedimentary rocks.
Stratification
42
are large scale reflection of transport of gravel and sand by currents that flow over the sediment surface (river channels). Sediment is moved up and eroded along a gentle up-current slope, re-deposited on the down current slope
CROSS-BEDDING
43
when the grain size within a bed decreases upwards. Commonly associated with turbulent suspension flows, they are initiated by slope failure, or earthquake that triggers down slope movement of sediment.
GRADED BEDDING
44
produced by flowing water or wave action, similar to cross-bedding, only on a smaller scale
RIPPLE MARKS
45
form when a water rich in mud dries out on the air.
MUD CRACKS
46
when remains of a number of biologically-created organisms exist in a sedimentary structure
FOSSILS
47
contain the actual organism remain
BODY FOSSILS
48
contain geological records of a biological activity (footprint, burrows, imprints)
TRACE FOSSILS
49
Example of Continental Depositional environments (4)
Alluvial, Aeolian, fluvial and Lacrustine
50
Example of Transitional Depositional Environments (3)
Deltaic Lagoonal Beach
51
Example ofMarine Depositional Environments
Shallow Water Marine Deep water marine Reef
52
Types of sedimentary environments
Continental, Depositional, marine, evaporite, glacial, volcanic
53
– is loose, unconsolidated environment which has been eroded, reshaped by water into another form and re-deposited in a non-marine setting
Alluvial (Alluvium, Alluvial Fan)
54
similar to alluvial fan, but deposition is via action of wind. Also known as dunes.
Aeolian (Eolian)
55
processes associated with rivers and streams and the deposits and landforms created by them.
Fluvial
56
water localized in a basin, surrounded by land apart, may or maybe connected by any river or other outlet. Also known as lakes.
Lacustrine
57
landform formed at the mouth of a river, where the river flows into an ocean, sea, estuary, lake or reservoir. Generally characterized by deposits of sediments.
Delta (River delta)
58
similar to lacustrine environment, except that it is a shallow body of water and it is separated from a larger body of water by small landmasses, barrier islands or reefs.
Lagoonal
59
landform along the coast of an ocean, sea or lake, or river.
Beach