otázka |
odpověď |
What is a crevasse splay? začněte se učit
|
|
A sedimentary fluvial deposit when a stream breaks it's levees and deposits onto a floodplain
|
|
|
What are alluvial rivers? What other river category is there? začněte se učit
|
|
Those flowing across their own deposits. The other category is incised rivers, which flow within eroded valleys
|
|
|
začněte se učit
|
|
subdivision of the stratigraphic record into mappable rock bodies on the bases of it's bounding discontinuities
|
|
|
Describe the graded river profile začněte se učit
|
|
A graded longitudinal profile of a river is the natural shape it assumes due to the dynamic balance between water and sediment - stepper at the source, flattening to a fraction of a degree at the mouth
|
|
|
začněte se učit
|
|
A curve of deepest points along the channel
|
|
|
začněte se učit
|
|
A narrow channel cutting off a point bar from the bank
|
|
|
začněte se učit
|
|
A lake created by an abandoned meander
|
|
|
What are allogeneic processes? And autogenic? začněte se učit
|
|
For a given depositional system, allogeneic processes are those which act outside of the system and affect the stratigraphic sequence, whereas autogenic are the internal ones
|
|
|
začněte se učit
|
|
It is a crescent-shaped depositional feature made of well sorted alluvial deposit accumulated at the inside bend of a river.
|
|
|
What is a microscopic heterogeneity in a fluvial deposit? začněte se učit
|
|
A porosity-permeability variation
|
|
|
What is a mesoscopic heterogeneity in a fluvial deposit? začněte se učit
|
|
Variation between bedding units and sedimentary structures
|
|
|
What is a macroscopic heterogeneity in a fluvial deposit? začněte se učit
|
|
Variability associated with the deposition of channels and bars
|
|
|
What is a megascopic heterogeneity in a fluvial deposit? začněte se učit
|
|
Variations across major sedimentary units and entire basins
|
|
|
začněte se učit
|
|
Because of turbulence, internal shear forces and bank-bed friction
|
|
|
How is a bottom of a straight channel shaped and why začněte se učit
|
|
There is a sinuous thalweg with alternate bars on the insides of it's bends, due to the same factors that cause point bars in meandering to rivers
|
|
|
What factors lead to a braided river? začněte se učit
|
|
Increased discharge, high discharge variations, higher slope, presence of coarse non-cohesive sediment which the river is unable to carry (may be brought suddenly due to a major flood or volcanic eruption)
|
|
|
How is sinuousity defined? začněte se učit
|
|
A ratio of the curvilinear and straight distance between two points
|
|
|
Which characteristics of single-thread and anastomosed rivers stand out in comparison with meandering and braided? začněte se učit
|
|
Low sinuousity, narrow channels (stable stream position), typically found on broad low-slope plains
|
|
|
Where do anastomosed rivers form? začněte se učit
|
|
In areas of rapid aggradation, such as confined, rapidly subsiding basins or where rapid base-level rise is matched by an abundant sediment supply.
|
|
|
How does bank vegetation influence channel evolution? začněte se učit
|
|
It stabilizes the bank, inhibits braiding and prevents flooding
|
|
|
How can a dam affect the river? začněte se učit
|
|
It reduces discharge variability, often leading to a development of a meandering style
|
|
|
How are mid-channel braid bars formed? začněte se učit
|
|
Outside of gentle bends in the thalweg, by a similar process as in point bar formation
|
|
|
What is the definition of a bedload? začněte se učit
|
|
Larger grains which are moved by sliding or rolling along the bed
|
|
|
How does a debris flow deposit look like? začněte se učit
|
|
Poorly sorted, contains large pebbles, cobbles or even boulders mixed together, embedded in a sand-silt-clay matrix. The matrix may show subtle grading, while the clasts may show a preferred orientation imposed by internal shear in the last flow moments
|
|
|
What is river competence and what does it depend on? začněte se učit
|
|
It is the maximum grain size that can be transported, depends on velocity and depth of the flow
|
|
|
What is river capacity and what does it depend on? začněte se učit
|
|
The total volume of sediment that can be moved, it depends on the magnitude of discharge
|
|
|
What is a crevasse of a river? začněte se učit
|
|
|
|
|
začněte se učit
|
|
|
|
|
What is the difference between a current ripple and wave ripple? začněte se učit
|
|
The former is asymmetrical (stepper on the lee side), the latter symmetrical
|
|
|
Characterize trough cross-stratification začněte se učit
|
|
In sections parallel to the flow we have curved planar erosional surfaces separating sets of foreset laminae. In perpendicular sections bowl-shaped trough surfaces separate concordant concave laminae. Formed by migration of ripples with irregular crests.
|
|
|
Characterize planar cross-stratification začněte se učit
|
|
In a section parallel to the flow we have flat erosional surfaces separating foreset laminae. In a perpendicular section laminae are flat and horizontal. Formed by migration of ripples with straight crests.
|
|
|
What is the difference between fluvial ripples and fluvial dunes/megaripples? začněte se učit
|
|
They are respectively smaller and larger than 5 cm in height. Dunes have larger wavelengths, may be covered by smaller ripples and they correspond to higher Froude numbers
|
|
|
What are upper flow regime bedforms and what stratigraphic record do they leave? začněte se učit
|
|
Froude number close to 1: upper plane bed, leaving horizontal laminae. Fr>1: antidunes, small upstream migrating bedforms that do not get preserved in the stratigraphic record
|
|
|
How to identify the growth of an active point bar? začněte se učit
|
|
Succession of vegetation - the oldest part will have trees, younger grass, youngest will be bare
|
|
|
What are floodplain deposits like? začněte se učit
|
|
Mainly fine grained clastic units
|
|
|
What is the process of avulsion? začněte se učit
|
|
Permanent diversion of a channel through a crevasse, if it has built up an alluvial ridge and the diversion results in a slope advantage for the channel
|
|
|
What is a perennial river? začněte se učit
|
|
A river which flows all year round
|
|
|
How do outcrops in ephemeral arid environment braidplains look like? začněte se učit
|
|
Tabular sandstone bodies several meters thick, consisting of plane-laminated sandstone. Or flood sheets comprising thinning and fining upward assemblages of cross-bedding and ripples
|
|
|
How could an outcrop of a braided river in an arid gravel-dominated environment look like? začněte se učit
|
|
Graded bedding of large grains due to size sorting during transportation. Or poorly sorted deposits from violent debris flows.
|
|
|
What depositional sequence is typical in alluvial settings and why? začněte se učit
|
|
Fining-upward. Aggradation of a channel results in decreasing flow depth and velocity, and consequently in a decrease in the competency and capacity of the flow. Development of point bars also tends to follow a fining-upward trend
|
|
|
What are thick sandstone sheets in alluvial settings like and what could they be attributed to? začněte se učit
|
|
4-16 m thick, possibly extending for many kilometers. They may reflect allogeneic causes such as gentle basin tilting or base level change
|
|
|
How does sediment deposit look like in ephemeral streams? začněte se učit
|
|
They are accumulated in flash floods, forming successions of stacked fining-upward sandstone sheets
|
|
|
What does a coarsening-upward sequence in proximal alluvial deposits indicate? How is it called and how big can it be? začněte se učit
|
|
It is a record of increasing source-area relief and depositional slope during tectonism (allogenic factor). It is referred to as tectonic cyclotherm and can be up to hundreds of meters thick and basin-wide
|
|
|
What is the concept of accommodation in stratigraphy? začněte se učit
|
|
The space available for sedimentation and how this volume changes in response to allogenic forces
|
|
|
What is an eustatic sea-level? začněte se učit
|
|
Distance from center of the Earth to the sea surface
|
|
|
What happens to the river when the base level drops? začněte se učit
|
|
If the exposed slope is steeper than river's graded profile, the river will erode its bed developing an incised valley. If the slope is more gentle, the river will increase sinuousity. If the river carries lots of sediment it may prograde and not incise.
|
|
|
What happens to a river valley during a stable sea-level period? začněte se učit
|
|
The valley will widen, which can be preserved in the form of terrace remnants along the valley walls
|
|
|
What does a sequence boundary represent in non-marine systems? začněte se učit
|
|
The final position of the subaerial erosion surface immediately prior to the commencement of a new phase of base-level rise
|
|
|
What happens to incised valleys during base-level rise? začněte se učit
|
|
|
|
|
How does base-level rise affect alluvial deposition? začněte se učit
|
|
A decrease in slope in the lower course of the river leads to a reduction of competency and, consequently, in the grain size of the sediment transported and deposited
|
|
|
What is an alloformation sequence related to base-level changes? začněte se učit
|
|
FSST (falling-stage systems tract) -> SB (sequence boundary) -> LST (lowstand systems tract) -> TST (transgressive systems tract) -> MFS (maximum flooding surface) -> HST (highstand systems tract) -> SB
|
|
|
How is the maximum flooding surface reflected in stratigraphy? začněte se učit
|
|
Marine influence on typically fluvial deposits. Possible tidal influence (tidal bedding, reversing cross-bedding, sigmoidal bedding...)
|
|
|
Why is there no erosion surface within coastal fluvial systems which would correspond to lowstand erosion? začněte se učit
|
|
Because such surfaces are continually modified by channel scour, even during transgression
|
|
|
What happens to a channel during a transition from cold to warm phase? How about the other way? začněte se učit
|
|
Incision, because discharge increases while sediment yield is low. Rivers of anastomosing and meandering style tend to develop. The other way as well, except the discharge increase is not due to melting snow but reduced evapotranspiration.
|
|
|
Which river style develops in glacial and interglacial periods, respectively? začněte se učit
|
|
Glacial - braided. Interglacial - meandering
|
|
|
How are sedimentary rocks formed? začněte se učit
|
|
Weathering of source rock, transportation (water, wind, mudflow, glacier etc.), deposition and lithification (cementing, compacting), or direct precipitation (e g evaporites, reefs)
|
|
|
začněte se učit
|
|
|
|
|
How do mudstone-sandstone-carbonates proportions differ between the outcrop statistics and bulk chemistry of the Earth's crust? Why? začněte se učit
|
|
Mudstone constitutes ~50% of the outcrops but it should be ~80% based on crust chemistry based estimations (sandstones/carbonate make up the rest in ~3/2 ratio). Reason: mudstones may preferentially land on oceanic floors.
|
|
|
What are terrigenous clastic rocks? začněte se učit
|
|
Sedimentary rocks formed from clasts of particles (blocks/boulders/cobbles/pebbles/granules/sand/silt/clay) with a fragmental texture (discrete grains in tangential contact with each other)
|
|
|
What are rudites? What other categories are there? začněte se učit
|
|
Rudites are sedimentary rocks with gravel-sized (>~2 mm) grains. Other categories are arenite (sand grains) and lutite (clay grains)
|
|
|
What are the two main rudite types and what are their characteristics? začněte se učit
|
|
Breccias (angular clasts) and conglomerates (more rounded grains)
|
|
|
začněte se učit
|
|
A fine-grained sedimentary rock characterized by fissibility, which is the tendency to break into thin slabs along it's laminations
|
|
|
začněte se učit
|
|
Above 256 mm: boulders, 64-256 mm: cobbles, 4-64 mm: pebbles, 2-4 mm: granules; 1/16 - 2 mm: sand, 1/256 - 1/16 mm: silt; below 1/256 mm: clay
|
|
|
začněte se učit
|
|
Φ = -log_2(S), where S is grain size in millimeters
|
|
|
What is a measure of grain sorting? začněte se učit
|
|
Standard deviation of the grain size distribution
|
|
|
Which environments is well rounded and angular sand typical for, respectively? začněte se učit
|
|
Well rounded: eolian, nearshore (surf zone). Angular: glacial, turbidity currents
|
|
|
What is the difference between detrital and authigenic minerals? What are the examples of each category? začněte se učit
|
|
Detrital (quartz, feldspar) survive weathering and are transported in sediment grains. Authigenic (gypsum, halite) form in-situ in the depositional site in response to geochemical processes
|
|
|
Definition and examples of penecontemporaneous sedimentary structures začněte se učit
|
|
Created not during, but shortly after deposition. Examples: load casts, mud cracks
|
|
|
Definition and examples of primary sedimentary structures začněte se učit
|
|
Created during deposition. Examples: graded bedding, cross-bedding, wave ripples
|
|
|
What's the difference between strata and laminae? začněte se učit
|
|
Thickness, the boundary is usually set at 1 cm
|
|
|
What are sole markings and what processes are responsible for their formation? začněte se učit
|
|
Structures formed in the bottom of a bed by: 1) uneven weight distribution upon a softer (mud) layer (load casts), 2) current action reworking the mud surface, 3) activities of living organisms on that surface
|
|
|
Genesis-based subcategories of rudites začněte se učit
|
|
Epiclastic (physical disintegration or weathering of preexisting rocks), pyroclastic (explosive volcanic activity), cataclastic (local Earth movements or solution phenomena), meteoritic (extraterrestrial)
|
|
|
Volume % of sub-2 mm particles in conglomerates začněte se učit
|
|
Clast-supported: <15%, matrix-supported: 15-80%
|
|
|
What are orthoconglomerates and paraconglomerates? začněte se učit
|
|
Synonyms for clast-supported and matrix-supported conglomerates
|
|
|
How are conglomerates classified based on rock type composition? začněte se učit
|
|
Monomict - one type of rock, polymict - different types of rock
|
|
|
How does wind velocity change with height? začněte se učit
|
|
Increases logarithmically
|
|
|
What types of wind entrainment are there? začněte se učit
|
|
Reptation / creep (rolling, sliding along the ground) for largest grains, saltation for sand sized particles, suspension for dust (which can also be entrained secondarily by impact of salting sand grains)
|
|
|
What is friction velocity and how does it depend on grain size? začněte se učit
|
|
The minimal wind velocity needed to pick up (entrain) a particle. It has a minimum (~50-500 μm) - for small particles it's harder because of cohesion (~d^(-3)), for big harder because of gravity
|
|
|
Dune types and corresponding wind directions začněte se učit
|
|
Perpendicular: barchan - thin sides ahead, barchanoid - chain of barchans, transverse - barchans merged into undulating linear, parabolic - thick sides ahead, thin held by vegetation. Parallel: longitudinal (seif). Varied directions: star dunes
|
|
|
What is the difference between eolian ripple and dune? začněte se učit
|
|
|
|
|
What are granule ripples? začněte se učit
|
|
Coarse grained ripples built on bedrock by reptation. Observed for example on Meridiani Planum
|
|
|
What are eolian dunes composed of (chemically) začněte se učit
|
|
On Earth: predominantly quartz, sometimes gypsum or basaltic in playa and volcanic environments, respectively. On Mars: basaltic, mafic composition
|
|
|
How are eolian dunes preserved in stratigraphic record? začněte se učit
|
|
Sandstones with cross-bedding at ~30° angle (angle of repose)
|
|
|
What are the dimensions of dust particles on Mars and Earth? začněte se učit
|
|
|
|
|
Why does Mars appear red? začněte se učit
|
|
Presence of iron oxides in basaltic dust grains
|
|
|
How are dust devils created? začněte se učit
|
|
Lifting of dust particles by a vortex of thermal flux from surface heating by the Sun. Usually form in the afternoon, when the surface has been sufficiently heated
|
|
|
začněte se učit
|
|
It is a thick deposit of wind-blown dust, forming an accumulation of loosely cemented clay, silt and sand, held together by cohesion. Often formed in periglacial settings (side edges of glaciers)
|
|
|
začněte se učit
|
|
A rock modified by wind abrasion, typically with one flat side due to blasting sand
|
|
|
začněte se učit
|
|
Elongated hills with one (windward) side almost vertical. Sculpted by blasting of sand carried by a monodirectional wind, take thousands of years to form. Dimensions vary from centimeters to kilometers
|
|
|
začněte se učit
|
|
A shallow, linear feature of different albedo due to deposition/erosion/protection from deposition near an obstacle in an environment with a prevalent wind direction
|
|
|
What are characteristics of distal depositional environments that set them apart from proximal? začněte se učit
|
|
Well sorted and well rounded sediment, rarity of large particles, transformation of feldspar to other minerals, less dependence on source area
|
|
|
When and why are buildings likely to collapse in earthquakes? začněte se učit
|
|
If they are standing on mud(stone), the mud becomes liquified (water entering pores) in the earthquake
|
|
|
Examples of laminar to turbulent flow transitions observed in real life začněte se učit
|
|
Water coming out from a tap or smoke coming out from a candle
|
|
|
Describe the Reynolds number concept začněte se učit
|
|
It is a ratio of inertial (d•v^2•l^2) and viscous forces (u•v•l), so Re=v•l•d/u, where v - velocity of the flow, l - flow cross-section, d - fluid density, u - fluid viscosity. Critical value of laminar-turbulent transition ain't fixed, but €[2000,3500]
|
|
|
Describe the Hjulström diagram začněte se učit
|
|
It defines areas in the parameter space of river flow velocity and grain size for which grains are: A) Deposited (threshold a bit above 0.01 mm, higher speed limits for bigger grains) B) transported, C) eroded (minimum speed at ~0.1 mm due to cohesion)
|
|
|
začněte se učit
|
|
A ratio of flow velocity v and a velocity of a contained wave √(g•l), where g is gravitational acceleration and l the flow depth. A value of 1 is considered to be critical
|
|
|
How does mud content affect debris on a slope? začněte se učit
|
|
As little as 5-10% can trigger a debris flow
|
|
|
What's the difference between a fluvial channel and fluvial valley? začněte se učit
|
|
Channel: the place where a river actively flows. Valley: depression formed by prolonged action of rivers (larger)
|
|
|
What's the key difference between braided and anastomosing channels? začněte se učit
|
|
Anastomosing channels do not migrate but keep the same location year after year
|
|
|
začněte se učit
|
|
snowfields, valley glaciers, ice caps, ice sheets, floating ice (incl. icebergs), ice formed on lake surfaces, ground ice (permafrost)
|
|
|
Characterize a periglacial zone začněte se učit
|
|
An edge zone of a glacier where it is too dry or slightly too warm for the glacier to grow. Dominated by freeze-thaw cycles and deep-freezing of groundwater to form ground ice. Considerable potential for eolian processes to carry sediment such as loess
|
|
|
What is the difference between mountain glaciers and polar ice sheets in terms of sediment transportation? začněte se učit
|
|
The former move over bedrock, the latter over thick beds of soft sediment. Therefore, the ice sheets transport much more sediment
|
|
|
How is glacial ice formed? začněte se učit
|
|
Through repeated cycles of partial melting, referring and recrystallization. An intermediate stage between snow and ice, firn, has density greater than 0.5 g/cm^3. Final product of glacial ice reaches density of 0.9 g/cm^3 through further crystallization
|
|
|
How long does it take for glacial ice to form? začněte se učit
|
|
A few years in temperate areas. Hundreds of years in colder, dryer Antarctic areas
|
|
|
Describe the two zones of a glacier which are delineated by an equilibrium line začněte se učit
|
|
Accumulation zone: the mass of ice gained each year is greater than the mass lost by melting. Ablation zone: the other way around, at lower elevations and associated warmer temperatures.
|
|
|
What is and how to find out where is the equilibrium line of a glacier? začněte se učit
|
|
A location where there is neither gain nor loss of ice (averaged over ~1yr timescales). Can be approximated by the position of a snow line visible on a glacier at the end of the summer melt season.
|
|
|
Which factors besides gravity affect the downward creep ice movement along a glacier? začněte se učit
|
|
Thickness of the ice (increased shear stress) and temperature (ice close to the melting point can move faster (lower viscosity))
|
|
|
Where is most of the sedimentary record from Pleistocene glaciations preserved? začněte se učit
|
|
|
|
|
Where (in Alaska or Antarctica) do glaciers erode and transport more sediment and why? začněte se učit
|
|
In Alaska, because it's warmer and the temperature at the base of a glacier is close to the melting point at the pressure at the base. This also facilitates aggregation of refrozen ice debris that further boosts ability to erode
|
|
|
How is a roche moutonnée formed? začněte se učit
|
|
Abrasion of bedrock by a glacier on the stoss (upstream) side and plucking on the lee (downstream) side, resulting in a vertical wall on the lee side
|
|
|
Which various processes can lead to poorly sorted deposits? začněte se učit
|
|
Glaciers, landslides, pyroclastic flows, lahars, post-impact fallbacks
|
|
|
začněte se učit
|
|
A volcanic mudflow, composed out of a slurry of pyroclastic material, rocky debris and water. Can be fast, deep and destructive
|
|
|
začněte se učit
|
|
Any poorly sorted deposit (matrix-supported conglomerate), regardless of origin
|
|
|
začněte se učit
|
|
A diamict formed by aggregation and direct deposition of debris transported by glacial ice
|
|
|
What kinds of till are there? začněte se učit
|
|
Melt-out (debris released from melting ice), lodgement (smearing debris from melting glacier base into bedrock) and deformation (shearing and mixing of preexisting sediment, most effective)
|
|
|
What is the most widely accepted theory about drumlin formation? začněte se učit
|
|
Either erosional streamlining of preexisting sediment or selective deposition of thick units of deformation till
|
|
|
What's the difference between drumlins and flutes? začněte se učit
|
|
Flutes are thinner and less likely to be preserved
|
|
|
začněte se učit
|
|
During ice retreat, when the subglacial channels where water used to flow rapidly become choked with sediment
|
|
|
What is the flow in glaciers like? začněte se učit
|
|
|
|
|
How does the material in glaciers respond to deformation? začněte se učit
|
|
Upper layer is brittle, lower ductile
|
|
|
What is a cirque and what happens if multiple form close to each other? začněte se učit
|
|
A cirque is a concave amphitheater-shaped valley formed by glacial erosion. If two come next to each other, an arête (narrow ridge) is formed in between. If three or more converge, they meet at a horn (sharp peak)
|
|
|
začněte se učit
|
|
They are isolated summits or ridges protruding out from glaciers, often forming pyramidal peaks
|
|
|
začněte se učit
|
|
Debris pulverized to silt-sized particles generated by mechanical grinding of bedrock by a glacier. It can turn river's or lake's color grey, brown, turquoise or even milky white
|
|
|
What is an outwash plain? začněte se učit
|
|
An outwash plain, sometimes called a sandur, is a plain formed from glaciofluvial deposits due to meltwater outwash at a terminus of a glacier. These deposits are not cohesive, that's why formed rivers braid and not meander
|
|
|
How do current ripples move? začněte se učit
|
|
Saltation moves the sand grains in a current. As the flow passes the crest the grains move faster above the crest than behind (Bernoulli's principle, less z => more v). This creates a vortex of reverse flow depositing grains at lee side
|
|
|
How deep do wave ripples form? začněte se učit
|
|
Up to half the wavelength
|
|
|
What shapes a wave ripple? začněte se učit
|
|
Circular motion of water at a base of a wave
|
|
|
What are the characteristics of alluvial fans? začněte se učit
|
|
Conical fan shape, regular slope (on Earth 1°-5°) and presence of multiple diverging channels on the surface
|
|
|
začněte se učit
|
|
A debris flow dominated by fine grains
|
|
|
Why is there a distinction between debris flows and concentrated flows? začněte se učit
|
|
In the former, debris and water form a viscous slurry, which can be considered a one-phase fluid. In the latter, the water and solid particles are two different phases needed to be analyzed separately
|
|
|
What decides if current ripples have straight crests or not? začněte se učit
|
|
Curvy crests are due to lateral components of a vortex, occurring in higher flow turbulence
|
|
|
Describe the two types of lava začněte se učit
|
|
Pahoehoe: lower viscosity, smooth, coming in a slow, laminar flow. After it cools down one can walk on it. A'a': rough, pieces of rock, further from the volcano and lower temperature (~1170°C)
|
|
|
začněte se učit
|
|
If there is no unconformity, vertically successive facies correspond to adjacent depositional environments
|
|
|
Compare atmospheres on Mars, Venus and Titan začněte se učit
|
|
Mars: 0.0062 bar, -23°C, CO_2 dominated. Venus: 86 bar, 480°C, CO_2 dominated. Titan: 1.5 bar, -180°C, N_2 dominated
|
|
|
What is considered arid and semi-arid land? začněte se učit
|
|
The amount of yearly precipitation in millimeters should be below 10× the average temperature or 10-20× for arid and semi-arid respectively. Or UNESCO aridity index - ratio between precipitation and evaporation below 1/4 for arid land
|
|
|
začněte se učit
|
|
Thin exposed rock in arid environment
|
|
|
začněte se učit
|
|
An isolated rock hill or mountain on a plain, formed by differential erosion
|
|
|
začněte se učit
|
|
A series of coalescing alluvial fans coming out on the front of a mountain range
|
|
|
začněte se učit
|
|
A very gently inclined erosional surface
|
|
|
Compare the ability of wind and water to entrain sediment začněte se učit
|
|
A water flow of 1 m/s has competence comparable to air flow of 30 m/s
|
|
|
Describe the division between ergs, sand sheets and regs začněte se učit
|
|
Ergs are areas with sandy dunes, which facilitate further accumulation of sand there. The remainder of a desert will be sand sheets (small ripples only) and regs (rocky desert pavement)
|
|
|
What is the grading in ripples in sand sheets and why? začněte se učit
|
|
Inverse grading because saltation is easier for coarser sand (less cohesion)
|
|
|
What kinds of alluvial fans are there? začněte se učit
|
|
Mass-flow dominated (debris flow) and stream-flow dominated (fluvial)
|
|
|
Coastal environment categories začněte se učit
|
|
Microtidal (tides under 2m), mesotidal (2-6 m), macrotidal (6-16m)
|
|
|
Tidal monthly cycles and related sedimentary record začněte se učit
|
|
Spring tide - full or new Moon, thicker sigmoidal layers. Neap tide - 90° Sun-Earth-Moon angle, smallest tides and thinnest sigmoidal layers
|
|
|
Describe the herringbone cross-stratification začněte se učit
|
|
Layers of foresets dipping in opposite direction, indicative of periodically changing flow directions in tidal areas. May be mistaken for 90° direction change without 3-dimensional information
|
|
|
Littoral zone subdivision začněte se učit
|
|
Supertidal - backshore (beach). Intertidal - foreshore (exposed at low tide, dominated by flat bed or antidunes). Subtidal: shoreface (where waves reach the base, including the surf zone), offshore (deeper, only deposits from major storms)
|
|
|
What's a berm in a coastal environment? How does berm formation depend on the season? začněte se učit
|
|
A sand or gravel ridge tens of centimeters high, formed by sediment brought by the bigger waves that got deposited above the normal sea level. Berms created in the winter are usually bigger than in the summer (stronger storm waves)
|
|
|
What is the most important coastal process at geologic time scales? začněte se učit
|
|
|
|
|
How is transgression defined? začněte se učit
|
|
Sea moving inward on the land (usually due to sea level rise or land subsidence)
|
|
|
začněte se učit
|
|
A long and high ridge made of sediments that were deposited as a strand plain (right at the coast) and then got preserved and moved landward through progradation
|
|
|
What's the difference between a marsh and a swamp? začněte se učit
|
|
A marsh has grass only, a swamp also trees such as mangroves
|
|
|
What happens to a barrier cutting off a lagoon when sea level rises? začněte se učit
|
|
It becomes submerged and either preserves it's shape or collapses to a drape. A new barrier and lagoon may form above
|
|
|
What mineral forms through diagenesis in nearshore deposits? začněte se učit
|
|
Glauconite (a type of phyllosilicate)
|
|
|
What is a strand plain and when is it formed? začněte se učit
|
|
Deposit building up at the shore, formed in wave-dominated environments (both transgressive and regressive)
|
|
|
When are estuaries formed? začněte se učit
|
|
In transgressive environments without excessive sediment supply. Can be both tide and wave dominated, in the latter case barrier island and lagoons may form.
|
|
|
How does an estuary/delta bring sediment to a basin? začněte se učit
|
|
If the inner sediment has higher density, it rolls down the basin floor. If the inner sediment has lower density than the outer one, it is suspended and then gradually drops.
|
|
|
What happens in coastal environments with very strong tidal power? začněte se učit
|
|
Tidal flats are formed instead of deltas or estuaries
|
|
|
How is the energy balance within an estuary? začněte se učit
|
|
Wave-dominated in the most seaward part, then more tidal energy and then more river energy
|
|
|
How are deltas different in polar environments? začněte se učit
|
|
They get reworked by sea ice pushing against them in the winter
|
|
|
What are listric faults in sedimentary rocks? začněte se učit
|
|
Faults which flatten as they get deeper, formed by creeping of the sediment, especially associated with tectonic compression or extension
|
|
|
Characterize climbing ripples začněte se učit
|
|
Formed by suspended sediment depositing on top of preexisting bedforms. Little to none stoss side erosion, consequently stoss side laminae can be seen. If there is deposition on the stoss side, they may take a sinusoidal shape
|
|
|
What's a flame structure? začněte se učit
|
|
Set of bowl-shaped laminations caused by the weight of overlying beds forcing the underlying beds to push through in water-saturated deposits
|
|
|
What is a piedmont glacier? začněte se učit
|
|
A large spread ice lobe associated with a terminus of a glacier. Glacial lakes can be formed after
|
|
|
What is hummocky cross-stratification and how is it formed? začněte se učit
|
|
Varying thickness of sandstone beds, formed by reworking by storms - above storm weather wave base but above fair weather wave base. If only concave indentations then it's called swaley cross-stratification
|
|
|
What is a playa and what other names are there? začněte se učit
|
|
A flat area with salt deposits, formed in a dried out lake (evaporation exceeded recharge), occasionally hosts some water (up to ~1 m after rain). Also known as sabkha, chott or salar
|
|
|
Are levees in a slope fan symmetrical? začněte se učit
|
|
No, because of the Coriolis effect
|
|
|
Evolution cycle of a delta začněte se učit
|
|
Progradation (river-dominated) => abandonment, transforming into wave-dominated system with barriers and lagoons => subsidence/transgression leads to drowning of the barrier into an inner shelf shoal => reoccupation
|
|
|
začněte se učit
|
|
Delta plain (visible sediment plain), delta front (boundary between plain and slope), delta slope, prodelta (fully submerged)
|
|
|
What are hemipelagic sediments? začněte se učit
|
|
Terrigenous fine-grained sediments in deep-water settings
|
|
|
What are the conditions needed to form a Gilbert-type delta? začněte se učit
|
|
Transport of bedload as far as the river mouth, sufficiently low river/basin depth ratio, inertia-dominated effluent diffusion
|
|
|
Delta categories based on profile začněte se učit
|
|
Hjulström-type (low inclination, so called shoal water profile), Gilbert-type (angle of repose), mouth-bar-type (deposits forming bars that coalesce to build delta front)
|
|
|
Delta prototypes based on feeder system začněte se učit
|
|
A) very steep gradient, unconstrained flows, mass flows; B) steep gradient, unstable channels, bedload dominated; C) moderate gradient, stable channels, bedload dominated; D) low gradient, very stable, suspension dominated
|
|
|
Categories of deltas based on feeder and basin density začněte se učit
|
|
Hypopycnal, homopycnal, hyperpycnal
|
|
|
Evolutionary stages of alluvial fans začněte se učit
|
|
Precursor - steep talus -> rockfalls, rock slides, rock avalanches -> debris flows -> sheet flows & channelized flows
|
|
|
začněte se učit
|
|
A succession of several sets
|
|
|
Describe volcanic and plutonic rocks začněte se učit
|
|
Volcanic are extrusive, with microscopic crystals, categories segregated based on increasing silica content are basalt, andesite, rhyolite. Plutonic are intrusive and have coarse crystals, analogous categories are gabbro, diorite, granite
|
|
|
začněte se učit
|
|
Subduction zone volcanism (mountain ranges), spreading center volcanism (rift), interplate volcanism (hot spots)
|
|
|
What is a toadstool in geology? začněte se učit
|
|
An undercut mushroom shaped rock pedestal attributed to wind erosion
|
|
|
What facilitates eolian dune formation? začněte se učit
|
|
Presence of local obstructions in the way of the wind
|
|
|