質問 |
答え |
What is a crevasse splay? 学び始める
|
|
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? 学び始める
|
|
Those flowing across their own deposits. The other category is incised rivers, which flow within eroded valleys
|
|
|
学び始める
|
|
subdivision of the stratigraphic record into mappable rock bodies on the bases of it's bounding discontinuities
|
|
|
Describe the graded river profile 学び始める
|
|
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
|
|
|
学び始める
|
|
A curve of deepest points along the channel
|
|
|
学び始める
|
|
A narrow channel cutting off a point bar from the bank
|
|
|
学び始める
|
|
A lake created by an abandoned meander
|
|
|
What are allogeneic processes? And autogenic? 学び始める
|
|
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
|
|
|
学び始める
|
|
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? 学び始める
|
|
A porosity-permeability variation
|
|
|
What is a mesoscopic heterogeneity in a fluvial deposit? 学び始める
|
|
Variation between bedding units and sedimentary structures
|
|
|
What is a macroscopic heterogeneity in a fluvial deposit? 学び始める
|
|
Variability associated with the deposition of channels and bars
|
|
|
What is a megascopic heterogeneity in a fluvial deposit? 学び始める
|
|
Variations across major sedimentary units and entire basins
|
|
|
学び始める
|
|
Because of turbulence, internal shear forces and bank-bed friction
|
|
|
How is a bottom of a straight channel shaped and why 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
Low sinuousity, narrow channels (stable stream position), typically found on broad low-slope plains
|
|
|
Where do anastomosed rivers form? 学び始める
|
|
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? 学び始める
|
|
It stabilizes the bank, inhibits braiding and prevents flooding
|
|
|
How can a dam affect the river? 学び始める
|
|
It reduces discharge variability, often leading to a development of a meandering style
|
|
|
How are mid-channel braid bars formed? 学び始める
|
|
Outside of gentle bends in the thalweg, by a similar process as in point bar formation
|
|
|
What is the definition of a bedload? 学び始める
|
|
Larger grains which are moved by sliding or rolling along the bed
|
|
|
How does a debris flow deposit look like? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
The total volume of sediment that can be moved, it depends on the magnitude of discharge
|
|
|
What is a crevasse of a river? 学び始める
|
|
|
|
|
学び始める
|
|
|
|
|
What is the difference between a current ripple and wave ripple? 学び始める
|
|
The former is asymmetrical (stepper on the lee side), the latter symmetrical
|
|
|
Characterize trough cross-stratification 学び始める
|
|
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 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
Succession of vegetation - the oldest part will have trees, younger grass, youngest will be bare
|
|
|
What are floodplain deposits like? 学び始める
|
|
Mainly fine grained clastic units
|
|
|
What is the process of avulsion? 学び始める
|
|
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? 学び始める
|
|
A river which flows all year round
|
|
|
How do outcrops in ephemeral arid environment braidplains look like? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
The space available for sedimentation and how this volume changes in response to allogenic forces
|
|
|
What is an eustatic sea-level? 学び始める
|
|
Distance from center of the Earth to the sea surface
|
|
|
What happens to the river when the base level drops? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
|
|
|
How does base-level rise affect alluvial deposition? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
Glacial - braided. Interglacial - meandering
|
|
|
How are sedimentary rocks formed? 学び始める
|
|
Weathering of source rock, transportation (water, wind, mudflow, glacier etc.), deposition and lithification (cementing, compacting), or direct precipitation (e g evaporites, reefs)
|
|
|
学び始める
|
|
|
|
|
How do mudstone-sandstone-carbonates proportions differ between the outcrop statistics and bulk chemistry of the Earth's crust? Why? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
Breccias (angular clasts) and conglomerates (more rounded grains)
|
|
|
学び始める
|
|
A fine-grained sedimentary rock characterized by fissibility, which is the tendency to break into thin slabs along it's laminations
|
|
|
学び始める
|
|
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
|
|
|
学び始める
|
|
Φ = -log_2(S), where S is grain size in millimeters
|
|
|
What is a measure of grain sorting? 学び始める
|
|
Standard deviation of the grain size distribution
|
|
|
Which environments is well rounded and angular sand typical for, respectively? 学び始める
|
|
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? 学び始める
|
|
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 学び始める
|
|
Created not during, but shortly after deposition. Examples: load casts, mud cracks
|
|
|
Definition and examples of primary sedimentary structures 学び始める
|
|
Created during deposition. Examples: graded bedding, cross-bedding, wave ripples
|
|
|
What's the difference between strata and laminae? 学び始める
|
|
Thickness, the boundary is usually set at 1 cm
|
|
|
What are sole markings and what processes are responsible for their formation? 学び始める
|
|
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 学び始める
|
|
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 学び始める
|
|
Clast-supported: <15%, matrix-supported: 15-80%
|
|
|
What are orthoconglomerates and paraconglomerates? 学び始める
|
|
Synonyms for clast-supported and matrix-supported conglomerates
|
|
|
How are conglomerates classified based on rock type composition? 学び始める
|
|
Monomict - one type of rock, polymict - different types of rock
|
|
|
How does wind velocity change with height? 学び始める
|
|
Increases logarithmically
|
|
|
What types of wind entrainment are there? 学び始める
|
|
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? 学び始める
|
|
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 学び始める
|
|
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? 学び始める
|
|
|
|
|
What are granule ripples? 学び始める
|
|
Coarse grained ripples built on bedrock by reptation. Observed for example on Meridiani Planum
|
|
|
What are eolian dunes composed of (chemically) 学び始める
|
|
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? 学び始める
|
|
Sandstones with cross-bedding at ~30° angle (angle of repose)
|
|
|
What are the dimensions of dust particles on Mars and Earth? 学び始める
|
|
|
|
|
Why does Mars appear red? 学び始める
|
|
Presence of iron oxides in basaltic dust grains
|
|
|
How are dust devils created? 学び始める
|
|
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
|
|
|
学び始める
|
|
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)
|
|
|
学び始める
|
|
A rock modified by wind abrasion, typically with one flat side due to blasting sand
|
|
|
学び始める
|
|
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
|
|
|
学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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 学び始める
|
|
Water coming out from a tap or smoke coming out from a candle
|
|
|
Describe the Reynolds number concept 学び始める
|
|
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 学び始める
|
|
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)
|
|
|
学び始める
|
|
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? 学び始める
|
|
As little as 5-10% can trigger a debris flow
|
|
|
What's the difference between a fluvial channel and fluvial valley? 学び始める
|
|
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? 学び始める
|
|
Anastomosing channels do not migrate but keep the same location year after year
|
|
|
学び始める
|
|
snowfields, valley glaciers, ice caps, ice sheets, floating ice (incl. icebergs), ice formed on lake surfaces, ground ice (permafrost)
|
|
|
Characterize a periglacial zone 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
|
|
|
Where (in Alaska or Antarctica) do glaciers erode and transport more sediment and why? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
Glaciers, landslides, pyroclastic flows, lahars, post-impact fallbacks
|
|
|
学び始める
|
|
A volcanic mudflow, composed out of a slurry of pyroclastic material, rocky debris and water. Can be fast, deep and destructive
|
|
|
学び始める
|
|
Any poorly sorted deposit (matrix-supported conglomerate), regardless of origin
|
|
|
学び始める
|
|
A diamict formed by aggregation and direct deposition of debris transported by glacial ice
|
|
|
What kinds of till are there? 学び始める
|
|
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? 学び始める
|
|
Either erosional streamlining of preexisting sediment or selective deposition of thick units of deformation till
|
|
|
What's the difference between drumlins and flutes? 学び始める
|
|
Flutes are thinner and less likely to be preserved
|
|
|
学び始める
|
|
During ice retreat, when the subglacial channels where water used to flow rapidly become choked with sediment
|
|
|
What is the flow in glaciers like? 学び始める
|
|
|
|
|
How does the material in glaciers respond to deformation? 学び始める
|
|
Upper layer is brittle, lower ductile
|
|
|
What is a cirque and what happens if multiple form close to each other? 学び始める
|
|
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)
|
|
|
学び始める
|
|
They are isolated summits or ridges protruding out from glaciers, often forming pyramidal peaks
|
|
|
学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
Up to half the wavelength
|
|
|
What shapes a wave ripple? 学び始める
|
|
Circular motion of water at a base of a wave
|
|
|
What are the characteristics of alluvial fans? 学び始める
|
|
Conical fan shape, regular slope (on Earth 1°-5°) and presence of multiple diverging channels on the surface
|
|
|
学び始める
|
|
A debris flow dominated by fine grains
|
|
|
Why is there a distinction between debris flows and concentrated flows? 学び始める
|
|
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? 学び始める
|
|
Curvy crests are due to lateral components of a vortex, occurring in higher flow turbulence
|
|
|
Describe the two types of lava 学び始める
|
|
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)
|
|
|
学び始める
|
|
If there is no unconformity, vertically successive facies correspond to adjacent depositional environments
|
|
|
Compare atmospheres on Mars, Venus and Titan 学び始める
|
|
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? 学び始める
|
|
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
|
|
|
学び始める
|
|
Thin exposed rock in arid environment
|
|
|
学び始める
|
|
An isolated rock hill or mountain on a plain, formed by differential erosion
|
|
|
学び始める
|
|
A series of coalescing alluvial fans coming out on the front of a mountain range
|
|
|
学び始める
|
|
A very gently inclined erosional surface
|
|
|
Compare the ability of wind and water to entrain sediment 学び始める
|
|
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 学び始める
|
|
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? 学び始める
|
|
Inverse grading because saltation is easier for coarser sand (less cohesion)
|
|
|
What kinds of alluvial fans are there? 学び始める
|
|
Mass-flow dominated (debris flow) and stream-flow dominated (fluvial)
|
|
|
Coastal environment categories 学び始める
|
|
Microtidal (tides under 2m), mesotidal (2-6 m), macrotidal (6-16m)
|
|
|
Tidal monthly cycles and related sedimentary record 学び始める
|
|
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 学び始める
|
|
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 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
|
|
|
How is transgression defined? 学び始める
|
|
Sea moving inward on the land (usually due to sea level rise or land subsidence)
|
|
|
学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
Glauconite (a type of phyllosilicate)
|
|
|
What is a strand plain and when is it formed? 学び始める
|
|
Deposit building up at the shore, formed in wave-dominated environments (both transgressive and regressive)
|
|
|
When are estuaries formed? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
Tidal flats are formed instead of deltas or estuaries
|
|
|
How is the energy balance within an estuary? 学び始める
|
|
Wave-dominated in the most seaward part, then more tidal energy and then more river energy
|
|
|
How are deltas different in polar environments? 学び始める
|
|
They get reworked by sea ice pushing against them in the winter
|
|
|
What are listric faults in sedimentary rocks? 学び始める
|
|
Faults which flatten as they get deeper, formed by creeping of the sediment, especially associated with tectonic compression or extension
|
|
|
Characterize climbing ripples 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
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? 学び始める
|
|
No, because of the Coriolis effect
|
|
|
Evolution cycle of a delta 学び始める
|
|
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
|
|
|
学び始める
|
|
Delta plain (visible sediment plain), delta front (boundary between plain and slope), delta slope, prodelta (fully submerged)
|
|
|
What are hemipelagic sediments? 学び始める
|
|
Terrigenous fine-grained sediments in deep-water settings
|
|
|
What are the conditions needed to form a Gilbert-type delta? 学び始める
|
|
Transport of bedload as far as the river mouth, sufficiently low river/basin depth ratio, inertia-dominated effluent diffusion
|
|
|
Delta categories based on profile 学び始める
|
|
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 学び始める
|
|
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 学び始める
|
|
Hypopycnal, homopycnal, hyperpycnal
|
|
|
Evolutionary stages of alluvial fans 学び始める
|
|
Precursor - steep talus -> rockfalls, rock slides, rock avalanches -> debris flows -> sheet flows & channelized flows
|
|
|
学び始める
|
|
A succession of several sets
|
|
|
Describe volcanic and plutonic rocks 学び始める
|
|
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
|
|
|
学び始める
|
|
Subduction zone volcanism (mountain ranges), spreading center volcanism (rift), interplate volcanism (hot spots)
|
|
|
What is a toadstool in geology? 学び始める
|
|
An undercut mushroom shaped rock pedestal attributed to wind erosion
|
|
|
What facilitates eolian dune formation? 学び始める
|
|
Presence of local obstructions in the way of the wind
|
|
|