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What is a crevasse splay? kezdjen tanulni
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A sedimentary fluvial deposit when a stream breaks it's levees and deposits onto a floodplain
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What are alluvial rivers? What other river category is there? kezdjen tanulni
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Those flowing across their own deposits. The other category is incised rivers, which flow within eroded valleys
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kezdjen tanulni
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subdivision of the stratigraphic record into mappable rock bodies on the bases of it's bounding discontinuities
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Describe the graded river profile kezdjen tanulni
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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
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kezdjen tanulni
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A curve of deepest points along the channel
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A narrow channel cutting off a point bar from the bank
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A lake created by an abandoned meander
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What are allogeneic processes? And autogenic? kezdjen tanulni
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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
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kezdjen tanulni
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It is a crescent-shaped depositional feature made of well sorted alluvial deposit accumulated at the inside bend of a river.
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What is a microscopic heterogeneity in a fluvial deposit? kezdjen tanulni
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A porosity-permeability variation
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What is a mesoscopic heterogeneity in a fluvial deposit? kezdjen tanulni
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Variation between bedding units and sedimentary structures
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What is a macroscopic heterogeneity in a fluvial deposit? kezdjen tanulni
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Variability associated with the deposition of channels and bars
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What is a megascopic heterogeneity in a fluvial deposit? kezdjen tanulni
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Variations across major sedimentary units and entire basins
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Because of turbulence, internal shear forces and bank-bed friction
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How is a bottom of a straight channel shaped and why kezdjen tanulni
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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
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What factors lead to a braided river? kezdjen tanulni
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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)
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How is sinuousity defined? kezdjen tanulni
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A ratio of the curvilinear and straight distance between two points
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Which characteristics of single-thread and anastomosed rivers stand out in comparison with meandering and braided? kezdjen tanulni
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Low sinuousity, narrow channels (stable stream position), typically found on broad low-slope plains
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Where do anastomosed rivers form? kezdjen tanulni
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In areas of rapid aggradation, such as confined, rapidly subsiding basins or where rapid base-level rise is matched by an abundant sediment supply.
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How does bank vegetation influence channel evolution? kezdjen tanulni
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It stabilizes the bank, inhibits braiding and prevents flooding
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How can a dam affect the river? kezdjen tanulni
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It reduces discharge variability, often leading to a development of a meandering style
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How are mid-channel braid bars formed? kezdjen tanulni
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Outside of gentle bends in the thalweg, by a similar process as in point bar formation
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What is the definition of a bedload? kezdjen tanulni
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Larger grains which are moved by sliding or rolling along the bed
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How does a debris flow deposit look like? kezdjen tanulni
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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
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What is river competence and what does it depend on? kezdjen tanulni
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It is the maximum grain size that can be transported, depends on velocity and depth of the flow
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What is river capacity and what does it depend on? kezdjen tanulni
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The total volume of sediment that can be moved, it depends on the magnitude of discharge
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What is a crevasse of a river? kezdjen tanulni
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kezdjen tanulni
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What is the difference between a current ripple and wave ripple? kezdjen tanulni
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The former is asymmetrical (stepper on the lee side), the latter symmetrical
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Characterize trough cross-stratification kezdjen tanulni
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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.
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Characterize planar cross-stratification kezdjen tanulni
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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.
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What is the difference between fluvial ripples and fluvial dunes/megaripples? kezdjen tanulni
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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
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What are upper flow regime bedforms and what stratigraphic record do they leave? kezdjen tanulni
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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
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How to identify the growth of an active point bar? kezdjen tanulni
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Succession of vegetation - the oldest part will have trees, younger grass, youngest will be bare
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What are floodplain deposits like? kezdjen tanulni
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Mainly fine grained clastic units
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What is the process of avulsion? kezdjen tanulni
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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
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What is a perennial river? kezdjen tanulni
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A river which flows all year round
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How do outcrops in ephemeral arid environment braidplains look like? kezdjen tanulni
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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
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How could an outcrop of a braided river in an arid gravel-dominated environment look like? kezdjen tanulni
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Graded bedding of large grains due to size sorting during transportation. Or poorly sorted deposits from violent debris flows.
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What depositional sequence is typical in alluvial settings and why? kezdjen tanulni
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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
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What are thick sandstone sheets in alluvial settings like and what could they be attributed to? kezdjen tanulni
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4-16 m thick, possibly extending for many kilometers. They may reflect allogeneic causes such as gentle basin tilting or base level change
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How does sediment deposit look like in ephemeral streams? kezdjen tanulni
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They are accumulated in flash floods, forming successions of stacked fining-upward sandstone sheets
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What does a coarsening-upward sequence in proximal alluvial deposits indicate? How is it called and how big can it be? kezdjen tanulni
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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
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What is the concept of accommodation in stratigraphy? kezdjen tanulni
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The space available for sedimentation and how this volume changes in response to allogenic forces
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What is an eustatic sea-level? kezdjen tanulni
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Distance from center of the Earth to the sea surface
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What happens to the river when the base level drops? kezdjen tanulni
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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.
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What happens to a river valley during a stable sea-level period? kezdjen tanulni
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The valley will widen, which can be preserved in the form of terrace remnants along the valley walls
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What does a sequence boundary represent in non-marine systems? kezdjen tanulni
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The final position of the subaerial erosion surface immediately prior to the commencement of a new phase of base-level rise
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What happens to incised valleys during base-level rise? kezdjen tanulni
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How does base-level rise affect alluvial deposition? kezdjen tanulni
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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
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What is an alloformation sequence related to base-level changes? kezdjen tanulni
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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
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How is the maximum flooding surface reflected in stratigraphy? kezdjen tanulni
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Marine influence on typically fluvial deposits. Possible tidal influence (tidal bedding, reversing cross-bedding, sigmoidal bedding...)
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Why is there no erosion surface within coastal fluvial systems which would correspond to lowstand erosion? kezdjen tanulni
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Because such surfaces are continually modified by channel scour, even during transgression
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What happens to a channel during a transition from cold to warm phase? How about the other way? kezdjen tanulni
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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.
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Which river style develops in glacial and interglacial periods, respectively? kezdjen tanulni
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Glacial - braided. Interglacial - meandering
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How are sedimentary rocks formed? kezdjen tanulni
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Weathering of source rock, transportation (water, wind, mudflow, glacier etc.), deposition and lithification (cementing, compacting), or direct precipitation (e g evaporites, reefs)
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How do mudstone-sandstone-carbonates proportions differ between the outcrop statistics and bulk chemistry of the Earth's crust? Why? kezdjen tanulni
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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.
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What are terrigenous clastic rocks? kezdjen tanulni
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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)
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What are rudites? What other categories are there? kezdjen tanulni
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Rudites are sedimentary rocks with gravel-sized (>~2 mm) grains. Other categories are arenite (sand grains) and lutite (clay grains)
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What are the two main rudite types and what are their characteristics? kezdjen tanulni
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Breccias (angular clasts) and conglomerates (more rounded grains)
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kezdjen tanulni
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A fine-grained sedimentary rock characterized by fissibility, which is the tendency to break into thin slabs along it's laminations
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kezdjen tanulni
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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
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kezdjen tanulni
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Φ = -log_2(S), where S is grain size in millimeters
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What is a measure of grain sorting? kezdjen tanulni
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Standard deviation of the grain size distribution
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Which environments is well rounded and angular sand typical for, respectively? kezdjen tanulni
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Well rounded: eolian, nearshore (surf zone). Angular: glacial, turbidity currents
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What is the difference between detrital and authigenic minerals? What are the examples of each category? kezdjen tanulni
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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
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Definition and examples of penecontemporaneous sedimentary structures kezdjen tanulni
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Created not during, but shortly after deposition. Examples: load casts, mud cracks
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Definition and examples of primary sedimentary structures kezdjen tanulni
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Created during deposition. Examples: graded bedding, cross-bedding, wave ripples
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What's the difference between strata and laminae? kezdjen tanulni
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Thickness, the boundary is usually set at 1 cm
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What are sole markings and what processes are responsible for their formation? kezdjen tanulni
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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
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Genesis-based subcategories of rudites kezdjen tanulni
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Epiclastic (physical disintegration or weathering of preexisting rocks), pyroclastic (explosive volcanic activity), cataclastic (local Earth movements or solution phenomena), meteoritic (extraterrestrial)
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Volume % of sub-2 mm particles in conglomerates kezdjen tanulni
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Clast-supported: <15%, matrix-supported: 15-80%
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What are orthoconglomerates and paraconglomerates? kezdjen tanulni
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Synonyms for clast-supported and matrix-supported conglomerates
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How are conglomerates classified based on rock type composition? kezdjen tanulni
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Monomict - one type of rock, polymict - different types of rock
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How does wind velocity change with height? kezdjen tanulni
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Increases logarithmically
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What types of wind entrainment are there? kezdjen tanulni
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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)
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What is friction velocity and how does it depend on grain size? kezdjen tanulni
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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
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Dune types and corresponding wind directions kezdjen tanulni
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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
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What is the difference between eolian ripple and dune? kezdjen tanulni
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What are granule ripples? kezdjen tanulni
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Coarse grained ripples built on bedrock by reptation. Observed for example on Meridiani Planum
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What are eolian dunes composed of (chemically) kezdjen tanulni
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On Earth: predominantly quartz, sometimes gypsum or basaltic in playa and volcanic environments, respectively. On Mars: basaltic, mafic composition
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How are eolian dunes preserved in stratigraphic record? kezdjen tanulni
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Sandstones with cross-bedding at ~30° angle (angle of repose)
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What are the dimensions of dust particles on Mars and Earth? kezdjen tanulni
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Why does Mars appear red? kezdjen tanulni
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Presence of iron oxides in basaltic dust grains
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How are dust devils created? kezdjen tanulni
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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
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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)
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A rock modified by wind abrasion, typically with one flat side due to blasting sand
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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
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kezdjen tanulni
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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
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What are characteristics of distal depositional environments that set them apart from proximal? kezdjen tanulni
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Well sorted and well rounded sediment, rarity of large particles, transformation of feldspar to other minerals, less dependence on source area
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When and why are buildings likely to collapse in earthquakes? kezdjen tanulni
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If they are standing on mud(stone), the mud becomes liquified (water entering pores) in the earthquake
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Examples of laminar to turbulent flow transitions observed in real life kezdjen tanulni
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Water coming out from a tap or smoke coming out from a candle
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Describe the Reynolds number concept kezdjen tanulni
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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]
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Describe the Hjulström diagram kezdjen tanulni
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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)
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kezdjen tanulni
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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
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How does mud content affect debris on a slope? kezdjen tanulni
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As little as 5-10% can trigger a debris flow
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What's the difference between a fluvial channel and fluvial valley? kezdjen tanulni
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Channel: the place where a river actively flows. Valley: depression formed by prolonged action of rivers (larger)
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What's the key difference between braided and anastomosing channels? kezdjen tanulni
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Anastomosing channels do not migrate but keep the same location year after year
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kezdjen tanulni
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snowfields, valley glaciers, ice caps, ice sheets, floating ice (incl. icebergs), ice formed on lake surfaces, ground ice (permafrost)
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Characterize a periglacial zone kezdjen tanulni
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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
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What is the difference between mountain glaciers and polar ice sheets in terms of sediment transportation? kezdjen tanulni
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The former move over bedrock, the latter over thick beds of soft sediment. Therefore, the ice sheets transport much more sediment
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How is glacial ice formed? kezdjen tanulni
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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
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How long does it take for glacial ice to form? kezdjen tanulni
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A few years in temperate areas. Hundreds of years in colder, dryer Antarctic areas
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Describe the two zones of a glacier which are delineated by an equilibrium line kezdjen tanulni
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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.
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What is and how to find out where is the equilibrium line of a glacier? kezdjen tanulni
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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.
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Which factors besides gravity affect the downward creep ice movement along a glacier? kezdjen tanulni
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Thickness of the ice (increased shear stress) and temperature (ice close to the melting point can move faster (lower viscosity))
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Where is most of the sedimentary record from Pleistocene glaciations preserved? kezdjen tanulni
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Where (in Alaska or Antarctica) do glaciers erode and transport more sediment and why? kezdjen tanulni
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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
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How is a roche moutonnée formed? kezdjen tanulni
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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
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Which various processes can lead to poorly sorted deposits? kezdjen tanulni
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Glaciers, landslides, pyroclastic flows, lahars, post-impact fallbacks
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kezdjen tanulni
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A volcanic mudflow, composed out of a slurry of pyroclastic material, rocky debris and water. Can be fast, deep and destructive
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Any poorly sorted deposit (matrix-supported conglomerate), regardless of origin
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A diamict formed by aggregation and direct deposition of debris transported by glacial ice
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What kinds of till are there? kezdjen tanulni
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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)
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What is the most widely accepted theory about drumlin formation? kezdjen tanulni
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Either erosional streamlining of preexisting sediment or selective deposition of thick units of deformation till
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What's the difference between drumlins and flutes? kezdjen tanulni
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Flutes are thinner and less likely to be preserved
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kezdjen tanulni
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During ice retreat, when the subglacial channels where water used to flow rapidly become choked with sediment
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What is the flow in glaciers like? kezdjen tanulni
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How does the material in glaciers respond to deformation? kezdjen tanulni
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Upper layer is brittle, lower ductile
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What is a cirque and what happens if multiple form close to each other? kezdjen tanulni
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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)
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kezdjen tanulni
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They are isolated summits or ridges protruding out from glaciers, often forming pyramidal peaks
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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
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What is an outwash plain? kezdjen tanulni
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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
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How do current ripples move? kezdjen tanulni
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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
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How deep do wave ripples form? kezdjen tanulni
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Up to half the wavelength
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What shapes a wave ripple? kezdjen tanulni
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Circular motion of water at a base of a wave
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What are the characteristics of alluvial fans? kezdjen tanulni
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Conical fan shape, regular slope (on Earth 1°-5°) and presence of multiple diverging channels on the surface
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kezdjen tanulni
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A debris flow dominated by fine grains
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Why is there a distinction between debris flows and concentrated flows? kezdjen tanulni
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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
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What decides if current ripples have straight crests or not? kezdjen tanulni
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Curvy crests are due to lateral components of a vortex, occurring in higher flow turbulence
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Describe the two types of lava kezdjen tanulni
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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)
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kezdjen tanulni
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If there is no unconformity, vertically successive facies correspond to adjacent depositional environments
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Compare atmospheres on Mars, Venus and Titan kezdjen tanulni
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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
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What is considered arid and semi-arid land? kezdjen tanulni
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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
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kezdjen tanulni
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Thin exposed rock in arid environment
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kezdjen tanulni
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An isolated rock hill or mountain on a plain, formed by differential erosion
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A series of coalescing alluvial fans coming out on the front of a mountain range
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A very gently inclined erosional surface
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Compare the ability of wind and water to entrain sediment kezdjen tanulni
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A water flow of 1 m/s has competence comparable to air flow of 30 m/s
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Describe the division between ergs, sand sheets and regs kezdjen tanulni
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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)
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What is the grading in ripples in sand sheets and why? kezdjen tanulni
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Inverse grading because saltation is easier for coarser sand (less cohesion)
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What kinds of alluvial fans are there? kezdjen tanulni
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Mass-flow dominated (debris flow) and stream-flow dominated (fluvial)
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Coastal environment categories kezdjen tanulni
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Microtidal (tides under 2m), mesotidal (2-6 m), macrotidal (6-16m)
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Tidal monthly cycles and related sedimentary record kezdjen tanulni
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Spring tide - full or new Moon, thicker sigmoidal layers. Neap tide - 90° Sun-Earth-Moon angle, smallest tides and thinnest sigmoidal layers
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Describe the herringbone cross-stratification kezdjen tanulni
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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
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Littoral zone subdivision kezdjen tanulni
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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)
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What's a berm in a coastal environment? How does berm formation depend on the season? kezdjen tanulni
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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)
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What is the most important coastal process at geologic time scales? kezdjen tanulni
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How is transgression defined? kezdjen tanulni
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Sea moving inward on the land (usually due to sea level rise or land subsidence)
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kezdjen tanulni
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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
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What's the difference between a marsh and a swamp? kezdjen tanulni
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A marsh has grass only, a swamp also trees such as mangroves
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What happens to a barrier cutting off a lagoon when sea level rises? kezdjen tanulni
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It becomes submerged and either preserves it's shape or collapses to a drape. A new barrier and lagoon may form above
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What mineral forms through diagenesis in nearshore deposits? kezdjen tanulni
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Glauconite (a type of phyllosilicate)
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What is a strand plain and when is it formed? kezdjen tanulni
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Deposit building up at the shore, formed in wave-dominated environments (both transgressive and regressive)
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When are estuaries formed? kezdjen tanulni
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In transgressive environments without excessive sediment supply. Can be both tide and wave dominated, in the latter case barrier island and lagoons may form.
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How does an estuary/delta bring sediment to a basin? kezdjen tanulni
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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.
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What happens in coastal environments with very strong tidal power? kezdjen tanulni
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Tidal flats are formed instead of deltas or estuaries
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How is the energy balance within an estuary? kezdjen tanulni
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Wave-dominated in the most seaward part, then more tidal energy and then more river energy
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How are deltas different in polar environments? kezdjen tanulni
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They get reworked by sea ice pushing against them in the winter
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What are listric faults in sedimentary rocks? kezdjen tanulni
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Faults which flatten as they get deeper, formed by creeping of the sediment, especially associated with tectonic compression or extension
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Characterize climbing ripples kezdjen tanulni
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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
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What's a flame structure? kezdjen tanulni
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Set of bowl-shaped laminations caused by the weight of overlying beds forcing the underlying beds to push through in water-saturated deposits
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What is a piedmont glacier? kezdjen tanulni
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A large spread ice lobe associated with a terminus of a glacier. Glacial lakes can be formed after
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What is hummocky cross-stratification and how is it formed? kezdjen tanulni
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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
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What is a playa and what other names are there? kezdjen tanulni
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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
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Are levees in a slope fan symmetrical? kezdjen tanulni
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No, because of the Coriolis effect
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Evolution cycle of a delta kezdjen tanulni
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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
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kezdjen tanulni
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Delta plain (visible sediment plain), delta front (boundary between plain and slope), delta slope, prodelta (fully submerged)
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What are hemipelagic sediments? kezdjen tanulni
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Terrigenous fine-grained sediments in deep-water settings
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What are the conditions needed to form a Gilbert-type delta? kezdjen tanulni
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Transport of bedload as far as the river mouth, sufficiently low river/basin depth ratio, inertia-dominated effluent diffusion
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Delta categories based on profile kezdjen tanulni
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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)
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Delta prototypes based on feeder system kezdjen tanulni
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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
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Categories of deltas based on feeder and basin density kezdjen tanulni
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Hypopycnal, homopycnal, hyperpycnal
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Evolutionary stages of alluvial fans kezdjen tanulni
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Precursor - steep talus -> rockfalls, rock slides, rock avalanches -> debris flows -> sheet flows & channelized flows
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A succession of several sets
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Describe volcanic and plutonic rocks kezdjen tanulni
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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
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kezdjen tanulni
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Subduction zone volcanism (mountain ranges), spreading center volcanism (rift), interplate volcanism (hot spots)
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What is a toadstool in geology? kezdjen tanulni
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An undercut mushroom shaped rock pedestal attributed to wind erosion
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What facilitates eolian dune formation? kezdjen tanulni
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Presence of local obstructions in the way of the wind
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