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