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Principle of Equifinality začněte se učit
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Different processes can produce similar landforms
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Factors affecting impact crater morphologies začněte se učit
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Intrinsic: projectile size, velocity and composition. Environmental: gravity, atmosphere, crust composition, volatile presence
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Why is the spatial distribution of known terrestrial impact craters not homogenous? začněte se učit
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Primarily due to different ages of the crust. Secondary factors are ease of identification in different environments etc.
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How often do impacts of large bodies occur? začněte se učit
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For a diameter of 1 km every 350 kyr or so. For diameters above 10 km every 150 Myr
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What causes central peak formation in impact craters? začněte se učit
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An abrupt transition from very high to low pressures at the sub-impact point
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What kind of impactors are there? začněte se učit
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Near Earth Objects, main belt asteroids, Kuiper belt and Oort cloud comets (difficult to predict)
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Crater formation stages for simple craters začněte se učit
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Schock wave at first contact => excavation and ejecta release => transient cavity (~1.5 times the final depth) => modification - partial filling with breccia lens including metal-rich material, ejecta drop down forming a blanket and an elevated crater rim
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Types of impact craters in terms of size začněte se učit
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Simple (on Earth up to 2km, on bodies with lower gravity the threshold is higher), complex (on Earth up to 100 km), multiring basins
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What additional morphologies occur in complex craters and multiring basins, compared to simple craters? začněte se učit
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Complex: terraced walls due to slumping and a central peak. Sometimes the central peak can be a ring. In multiring basins there are multiple concentric rings
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How does the angle of impact α affect crater shape? začněte se učit
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For α<45° there is no effect, for α>45° craters start becoming elongated and ejecta distribution loses symmetry
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začněte se učit
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A crater with a low ridge and lobate appearance along the ejecta blanket edge, indicative of mudflow-like movement of ejecta. This would be caused by liquification due to the shock wave as the impact penetrates down to ice-rich underground layers
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Has the flux of impactors hitting planetary bodies been constant in time? začněte se učit
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No, there was a heavy bombardment 4 Gyr ago. Another late heavy bombardment 3.8 Gyr ago is also hypothesized.
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What heat loss mechanisms are dominant on which planetary bodies? začněte se učit
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Plate tectonics on Earth. Heat pipe volcanism on Io (also on early Earth). Conduction on the Moon, Mercury and Mars. Venus is uncertain, some mix of all three.
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začněte se učit
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A convective connection between the core-mantle boundary and the surface of a planet, leading to release of molten magma
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What's the relationship between tectonics and volcanism? začněte se učit
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The boundaries between tectonic plates are hot areas where plumes are likely to occur. Example: the "Ring of Fire" - a collection of volcanoes above the subduction zones of the Pacific Plate
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What areas are suspected to be subject to active tectonism on Venus? začněte se učit
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Beta Regio (a probable rift zone), Ishtar Terra (potential convergent mountain-building zone). Besides, coronae are hypothesized to be plume leftovers.
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How do hypsometric distributions of Earth, Mars and Venus compare to each other? začněte se učit
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Earth's is bimodal (continents+oceanic floor). Both Venus and Mars have unimodal distributions, but on Venus most points are in a +-2 km range, whereas on Mars it's +-8 km
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Describe the composition of Moon's surface začněte se učit
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Anorthositic highlands and basaltic mares. The latter is due to exposure through impacts after the magna ocean froze - indeed, in the magna ocean mafic minerals must have sunk deeper when they crystallized before the felsic ones.
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začněte se učit
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Vertical displacement - normal fault due to extension and reverse fault due to compression. Horizontal displacement - strike-slip fault
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What kind of a landscape is formed from a few parallel normal faults? začněte se učit
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Either tilt blocks or horst& graben landscape (horst is the higher part)
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začněte se učit
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They are long vein-like ridges formed by tectonic compression, consisting (in cross-section) of a backclimb, wrinkle (peak), a lobate front and extended frontlimb. They are common on the Moon, also appear on Mars and Mercury
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začněte se učit
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Mostly in the past: an extensional phase around 3.8 and a contractional phase around 3.6 Gyr ago. (Mars shrinking and losing heat)
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What are compressional and dilation shear bands? How to spot them on Mars? začněte se učit
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Small (human sized) scale tectonic features caused by shear forces, compacting and extensional respectively. There is room for fluids to get in, so diagenesis can occur and make them more pronounced on color images of e g Mars
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Why is crater transient depth bigger than the final depth? začněte se učit
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Because ejecta partially fall back inside the crater and the walls may partially collapse too. Also the bottom material gets uplifted
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What is a characteristic feature of impact crater rims which does not apply to volcanic craters? začněte se učit
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Inverted stratigraphy (ejecta coming from a deeper layer but deposited on top).
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Physical division of Earth's interior začněte se učit
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Brittle lithosphere which forms tectonic plates (crust and uppermost mantle), ductile atenosphere on which the plates move (rest of the mantle)
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Magma generation mechanisms začněte se učit
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Residual heat from planet formation, decay of radioactive elements, tidal heating
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Types of basaltic volcanism začněte se učit
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Mid-oceanic ridges, hot spots related to plumes
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Describe shield volcanoes začněte se učit
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Low profile volcanoes formed by eruption of low viscosity basaltic lava
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začněte se učit
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Steep conical hills formed from loose pyroclastic material around a volcanic vent, usually related to basaltic volcanism
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začněte se učit
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Deposits resulting from giant basaltic volcanic eruptions, usually linked to plumes
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Describe composite volcanoes začněte se učit
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Also known as stratovolcanoes. Made of layers of high viscosity, felsic lava. Cone shaped. Examples include Mount Fiji and Iztaccihuatl
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začněte se učit
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Also known as supervolcanoes, they are large craters formed by collapsed surface rock into empty magma chambers
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začněte se učit
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Dome shaped protrusions formed by slow extrusion of high viscosity lava
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How are lava tubes formed? začněte se učit
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When a low viscosity lava flow develops a continuous hard crust over a still following pahoehoe lava stream
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What's a pyroclastic flow? začněte se učit
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A fast moving (~100 km/h or even more) current of hot gas and volcanic rock, coming down from a volcano
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What can be a source of water in a lahar? začněte se učit
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Molten snow from the top of a volcano?
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Describe maars and tuff rings začněte se učit
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Both are low-standing volcanoes with bowl-shaped craters around pyroclastic cones. In maars, the crater would be below surrounding ground level and would therefore often host a lake. In tuff rings above
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začněte se učit
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They are flat-topped, steep-sided mountains formed by volcanic eruptions occurring under glaciers / ice sheets
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začněte se učit
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Volcanoclastic accumulation of breccia with glass fragments formed by quenching of subglacial or submarine extrusion of lava
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Volcanic landforms on the Moon, Mars and Venus začněte se učit
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Moon - sinuous rilles, shield volcanoes. Mars - Olympus Mons with summit calderas, shield volcanoes, lahar deposits. Venus - pancake domes
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začněte se učit
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Eruption of volatiles (liquid water, ammonia, hydrocarbons) from under the ice on icy moons, driven by the same processes as magma formation on warmer bodies
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začněte se učit
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Landslides - rotational, translational and block slides. Rockfalls and topples. Debris/Earth flows and avalanches. Slumps and creeps
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Mass wasting driving factors začněte se učit
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Gravity, slope, material and presence of volatiles
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Estimation formula and typical values of the angle of repose začněte se učit
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arctan(f), where f is the friction coefficient, doesn't take into account cohesion etc. Values for fine sand are around 35°, for coarse sand around 40° and for pebbles 45°
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začněte se učit
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A geomorphological landform moving and looking similarly to glaciers, but dominated by rocks with some buried interstitial ice
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What do slopes of landslide area probability densities on planetary bodies tell us? začněte se učit
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The slope on Earth is ~-2.3, on Mars ~-1, meaning that bigger landslides occur more preferentially on the latter (maybe due to rock fracture size, maybe because there's no rainfall to trigger smaller ones)
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What is a typical trigger of terrestrial landslides? začněte se učit
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Rainfall. Also earthquakes, human activity (disruptions from road construction), and others
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What's the difference between subaerial and submarine landslides? začněte se učit
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The latter can travel much larger distances for given fall heights (i e given initial potential energies)
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Examples of mass wasting on Mars začněte se učit
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Landslides, small gullies (might involve water flows), aureole deposits around Olympus Mons (uncertain origin, maybe former submarine landslides)
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Examples of mass wasting on the Moon začněte se učit
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Landslides, boulder tracks
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How do landslides on Mercury and Moon compare to each other? začněte se učit
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The ones on Mercury are a bit smaller, maybe due to stronger gravity
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What determines the spatial distribution of deserts on Earth? začněte se učit
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Global air circulation, leading to high pressure zones near tropics and poles. Also mountain ranges with the mountain shadow effect
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začněte se učit
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Huge dunes with heights of over 100 m and wavelength of ~0.5-2.5 km
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začněte se učit
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~1-100 m/yr on Earth, ~1 m / martian year (3.7 yr) on Mars
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What types of dunes are usually highest? začněte se učit
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Star dunes, as they accumulate sand from every direction instead of moving
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What is a stokes surface and an associated erosional feature? začněte se učit
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In an arid environment with some groundwater present deep down, the Stokes surface separates wet and dry sediment. It may become partially exposed by wind action with a preserved rock in the middle, called blowout feature
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Where and how is a desert pavement formed? začněte se učit
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In areas where many pebbles/cobbles/boulders exist within the sand, by blowing away of the sand and the rocks remaining on top of each other
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Temperature ranges on Mars začněte se učit
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When do annual dust storms occur on Mars? začněte se učit
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During the northern hemisphere winter, which is when the planet is close to it's peryhelion
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začněte se učit
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Mounds of sand which may be degraded barchan dunes
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How can grain sizes be inferred from remote sensing of planetary surfaces? začněte se učit
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Based on thermal inertia calculated from infrared images
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Mars exploration in the 20th century začněte se učit
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1964 - Mariner 4, only pictured craters; 1972 - Mariner 9 and Viking 1 & 2 (orbiters and landers) show a variety of features including fluvial, 1996 - Pathfinder (Sojourner rover) and Mars Global Surveyor including MOLA and THEMIS
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How is the martian datum defined? začněte se učit
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An equipotential surface (based on topography) corresponding to the mean radius at the equator
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Which part of Mars has more subsurface ice? začněte se učit
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Mars exploration in the year 2003 začněte se učit
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ESA Mars Express (radar measurements of water under the ice, mineral identification with OMEGA spectrometer). Mars Exploration Rovers from NASA (Opportunity and Spirit, able to clean the surface of rocks and study with a microscope)
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Mars exploration in years 2006-2016 začněte se učit
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2006 - Mars Reconnaissance Orbiter with CTX, HiRISE, SHARAD radar (measuring layers in the northern polar ice cap). 2012 - Curiosity rover with nuclear power, precision landing, studying minerals in outcrops. 2016 - ESA EXO Mars, landing failed
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Why are landing sites close to equator favored for martian rovers? začněte se učit
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Mars exploration in the year 2020 začněte se učit
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NASA - Perseverance rover with the Ingenuity helicopter, aimed to collect samples and bring them back to Earth. China - Tianwen-1 mission with a rover, UAE - Hope mission
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Martian surface characteristics začněte se učit
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Bright areas are dusty, with dust including paragonite, hematite, volcanic material. Dark areas are basaltic
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When were valley networks on Mars formed? začněte se učit
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Characterize small gullies on Mars začněte se učit
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These gullies or troughs on slopes (preferentially poleward) may be due to melting ice or snow, but may also be due to dry flows of sand or CO_2 supported debris flows. Based on cross-cutting relationships they appear to be young - on the order of 10 Myr
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Examples of glacial landforms on Mars začněte se učit
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Eskers (sinuous sediment ridges) and kettles (depressions left by melting ice)
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Where did the Opportunity rover land and what did it find? začněte se učit
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It landed at Meridiani Planum and discovered hematite rich spherules known as blueberries
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Describe the transient martian ocean theory začněte se učit
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In the Hesperian oceans may have existed for ~100-1000 years, filled by outflow channel forming floods. Two possible shorelines have been identified but the outer one is far from equipotential line. May have been reworked by tsunamis and surface freezing
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Characteristics of the Noachian, Hesperian and Amazonian periods začněte se učit
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Noachian - heavy bombardment, valley network formation. Hesperian - volcanism, outflow channel formation, maybe oceans. Amazonian - late volcanism, low impact rates, late stage polar caps, cold and dry Mars
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How are boundaries between Noachian, Hesperian and Amazonian periods set? začněte se učit
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Based on crater counting. Absolute ages cannot be defined with certainty without direct sample analysis, but estimated around 3.7 Gyr for the Noachian/Hesperian and around 3.1 Gyr for the Hesperian/Amazonian boundary
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Formation hypotheses for Phobos and Deimos začněte se učit
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Either asteroid capture or an impact and coalescence of ejected debris
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Principle of uniformitarianism začněte se učit
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Natural laws do not change, but rates and intensities of processes can
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Describe the proposed formation scenario for martian "blueberries" based on the Utah analog začněte se učit
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They would be formed in a diagenetic concretion process in eolian/ playa environment. First hydrocarbon gas/fluid removes oxygen from oxides. Then water arrives and provides oxidizing conditions leading to precipitation of balls with hematite shells
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How are sandstone chimneys formed and why are they interesting for astrobiology? začněte se učit
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They form through groundwater sediment extrusion, fossilized fungi colonies have been found in Utah examples
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Address the topic of methane on Mars začněte se učit
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Trace amounts (on the order of ppb) have been found both through remote sensing and rover (Curiosity) measurements. Possible link with mud volcanoes. May have been formed biogenically,(bacteria) or diagenically (water -ock interactions)
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If there were oceans on Mars, why are there so few carbonates found there? začněte se učit
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SO_2 is more abundant on Mars, it's absorption in the water would make it acidic, inhibiting carbonate formation and forming sulfate rocks instead
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Describe a hydraulic jump začněte se učit
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Change of slope and depth shifts the Froude number above or below 1, making the flow super/sub critical and more or less erosive
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Why are fluvial dunes better preserved than eolian? začněte se učit
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They may contain larger grains, which cannot be moved by wind
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Reynolds numbers of gravity flows začněte se učit
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Low for debris flow, high for turbidity currents
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Describe the alluvial fan formation process začněte se učit
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The activity is happening only in some lobes, then dies out there and starts elsewhere (lobe switching). Channels incise in the upper part of the fan, deposit in the lower. A flow may be a debris flow, a sheet flow (more water & turbulence) or channelized
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začněte se učit
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Alluvial fans in arid areas, where the flow does out due to evaporation
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začněte se učit
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Alluvial fans directly transitioning to deltas due to the presence of a water body at the base of mountains. The Gilbert-type delta in the Jezero crater is considered an example
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River morphologies vs discharge and gradient slope začněte se učit
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Parallel downward lines separate straight/anastomosing, meandering and braided
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Water movement in a meandering river začněte se učit
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The flow is deeper and faster on the outer side of a meander
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What happens in a crevasse splay after the flooding? začněte se učit
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In arid environments water evaporates forming evaporite deposits. In humid areas standing water bodies can form and pedogenesis may be facilitated
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What is the problem with Noachian formation of fluvial valley networks? začněte se učit
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The atmosphere on Mars is not favorable for liquid water precipitation, and with the Sun having been 30% weaker back then should have been even less favorable
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Characteristics of sapping valleys začněte se učit
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Headward migration by collapsing walls, not well developed tributary system but mostly 1st order tributaries, similar depths of tributaries as the main valley, blunt amphitheater-shaped heads, structural control by fractures and tectonic levels.
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How can a lake in a crater be sustained during a dry season? začněte se učit
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By ground water flowing through the basaltic bedrock
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Types of ice age catastrophic floods začněte se učit
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Lake overbank spillage, ice impounding on a lake, sub-ice draining, subglacial water adding up to a lake, ice dam or sediment dam failure, subglacial volcanism (jökulhlaups)
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How fast was the water in the Channelled Scabland flood and where was it coming from? začněte se učit
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5-25 m/s, from the Glacial Lake Missoula and maybe also from under the northern ice sheet
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What do dry falls in the Channelled Scabland correspond to? začněte se učit
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Waterfalls in the waning stage of the flood
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How was the erosion ongoing in the Channelled Scabland? začněte se učit
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First loess was removed, then also some bedrock (differentially) by plucking and abrasion
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What other sources of outflow channels occur on Mars besides chaotic regions? začněte se učit
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Lakes in craters (e g Elaver Vallis), fracture zones (e g Athabasca Vallis from a fracture near Elysium, related to an active dyke that would have melted the ice, as supported by measurements from InSight)
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What has been inferred from the study of the topography of Simud Vallis? začněte se učit
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That it might have hosted a lake from which the water moved on to a potential northern ocean
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začněte se učit
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Triggered by an earthquake or impact, a wave gets bigger as it approaches the shore, several hits with the first one being the highest, able to capture destroy everything up to ~50 m high above sea level. Water velocity comparable to catastrophic floods
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Characteristic traces of tsunamis začněte se učit
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Lobate deposits of marine sandy sediment traveling uphill inland, gullies deepened by erosion left by a subsiding wave
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Arguments for shorelines on Mars začněte se učit
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Similar elevations of different deltas and outflow channel mouths, lobate tsunami like deposits (including the Viking 1 landing site near a potentially submarine crater) and herringbone cross-stratification found by the Chinese rover
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Where could liquid water exist in the martian surface today and why? začněte se učit
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Bottom of Hellas basin (highest pressure), only in the summer(sufficiently high temperature
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Why is there a lower bound on rampart crater sizes on Mars? začněte se učit
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Necessity to excavate groundwater present at a certain depth
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Difference between till and tillite začněte se učit
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Describe the snowball Earth model začněte se učit
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Based on diamictites in paleoequatorial outcrops a suspicion that Earth was fully glaciated several times in Precambrian, likely last time before life emerged
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Martian geomorphological features related to underground ice začněte se učit
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Hourglass features, debris aprons, debris covered glaciers at mid-latitudes
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Glacial landforms in the Tharsis rise začněte se učit
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Deposits on the north-western sides of the four major volcanoes, particularly big for Arsia Mons
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začněte se učit
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Mounds formed by pushing out of the soil by an ice lens forming over unfrozen ground
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Does Mars have Milankovitch cycles? How does it relate to the subsurface ice? začněte se učit
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Not quite, the moons are too small to stabilize the obliquity which displays large chaotic variations. Consequently, ice may have been deposited in some equatorial regions (Arabia Terra) in periods of high obliquity.
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What landform suggests former presence of ice in Valles Marineris? začněte se učit
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Large scale deep-seated gravitational spreading at tops of internal ridges, which could have been formed when surrounding and covering ice melted
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Polygonal feature dimensions in playa environments začněte se učit
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Smaller polygons at topographically lower areas, likely due to halite (which is soluble so travels to lower elevations in the water) inhibiting development of large polygon networks. Higher, as minerals change through gypsum to carbonates, larger polygons
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What do aligned spring mounds indicate? začněte se učit
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začněte se učit
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Transition of water-bearing sediment from a setting where clasts touch each other to the setting where they are separated by water
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How do clastic pipes form? začněte se učit
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1) Trigger from earthquake or impact leads to liquification of buried sediments 2) Liquified sediment squeezes out between non-liquified to form a sand volcano 3) Pipe cements, surroundings sink (removed base) 4) Erosion removes material around the pipe
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Largest clastic pipes on Earth and proposed origin začněte se učit
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~100 m in height and diameter, found in Utah. Maybe due to an impact, nearby Upheaval Dome might be a crater
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Where are mud volcanoes commonly found on Earth? začněte se učit
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Along orogenic belts, particularly in Azerbaijan, Pakistan, Japan
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Conditions needed for mud volcanoes začněte se učit
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Abundance of buoyant sediments, abnormally high rock porosity, high pressure gradient, a trigger such as an earthquake
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How does a mud volcano eruption look like? začněte se učit
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Release of mud, gas and oil. Resulting mudflow has a lot of gas bubbles inside and forms mud levees.
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What did we learn from chamber simulations of a hypothetical martian mud volcano eruption? začněte se učit
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In current martian conditions, mud would boil, erode a trench and freeze to a crust, creating structures similar to lava tubes
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Where are candidates for mud volcanoes found on Mars? začněte se učit
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A big cluster in the Chryse Planitia, also in other northern lowland areas such as Utopia Planitia (Chinese Zhurong rover came close), some in Valles Marineris
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How are mud volcanoes reflected in the stratigraphic record? začněte se učit
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Characteristics of remote sensing observations of potential martian mud volcanoes začněte se učit
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Low thermal inertia (contradicts magmatic alternative) and hematite spectral signatures along the rims (not occurring in terrestrial mud volcanoes)
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If the methane on Mars has formed in ancient times and is slowly being released, what is trapping it? začněte se učit
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Overlying ice or inclusion in CO_2 + CH_4 clathrate
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Compare lunar basalts to terrestrial začněte se učit
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Fe & Ti enriched, less viscous, higher melting temperature
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What is lunar mare formation dated for? začněte se učit
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Moon formation hypotheses other than impact and why were they dismissed začněte se učit
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Capture - unlikely for such a big body. Fission from Earth - would take too long. Accretion parallel with Earth - too different composition, particularly low iron content
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Tectonic features in lunar maria začněte se učit
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Grabens usually on the outer parts, wrinkle ridges closer to the central parts. Also influenced by gravity, including positive gravitational anomalies due to proximity to the mantle
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How do we know that the Moon is moving away from the Earth? začněte se učit
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Ancient tidal deposits indicate the tides used to be bigger. Nowadays we can also measure the subtle changes in the distance with lasers
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What observational evidence is there for the multi-stage filing of lunar maria with basalt? začněte se učit
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Ground penetrating radar measurements by the Japanese Kaguya mission showing layering with micrometeorite erosion caused regolith in between.
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Volcanic features on the Moon začněte se učit
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Suggested large and small shield volcanoes, sinuous rilles due to erosion by hot low viscosity lava, ring-moat dome structures clustered in maria due to extrusion of magmatic foam, skylights which may likely be lava tube openings
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What do we know about water on the Moon? začněte se učit
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May be brought by meteorites bearing ice. Likely preserved in deep craters in polar regions which are perpetually shaded, LCROSS mission intentionally crashed and detected a vapor plume. Remote sensing suggests OH in regolith, 1l of water from 1t regolith
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Apollo program highlights before Apollo 13 začněte se učit
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Apollo 8 - first flight of humans around the Moon. Apollo 10 - testing all procedures without actually landing. Apollo 11 - first human landing, 20.07.1969, Mare Tranquillitatis. Apollo 12 - landing near Surveyor 3 lander and approaching it by astronauts
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Apollo program highlights after Apollo 13 začněte se učit
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Apollo 15 - collecting samples from Hadley Rille, confirming lava flow origin. Apollo 16 - commander John Young flew to the Moon twice (before on Apollo 10). Apollo 17 - Harrison Schmidt as the only geologist who went to the Moon.
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začněte se učit
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Artemis II - analogous to Apollo 8. Artemis III - landing humans near the lunar south pole. Artemis IV - Gateway, lunar vehicle from Toyota, In-situ resource utilization (ilmenite (FeTiO_3, known from Apollo samples and remote sensing) and hopefully ice)
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Core volume fractions of inner Solar System planetary bodies začněte se učit
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Mercury 42%, Venus 12%, Earth 16%, Moon 4%, Mars 9%
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How many Mercurian days in a Mercurian year? začněte se učit
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začněte se učit
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Caloris Basin (1550 km diameter) and antipodal chaos, impact craters, intercrater plains, smooth plains (likely volcanic)
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Mercury volume change history začněte se učit
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First expansion which formed intercrater plains. Later, as the planet was cooling, shrinking leading to a 1-2 km radius decrease, evidenced by extensive thrust faults
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Evidence for volatiles on Mercury začněte se učit
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Mercury exploration history začněte se učit
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Mariner 10 -> 40 year hiatus -> Messenger -> BepiColombo (ESA/JAXA, arriving next year)
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Does the Mercury have a strong magnetic field? Why? začněte se učit
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Yes, likely because of the dynamo effect of the large core which is partially molten in the outer part
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Where can we find water on Venus? začněte se učit
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Only as vapor in the atmosphere, partial pressure 10 mbar
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What is the atmosphere on Venus like? začněte se učit
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Opaque in the optical because of sulfuric acid clouds. Lots of greenhouse gases: CO_2, SO_2, CO, HCl, water vapor (more in the past but it got subject to photodissociation: sunlight split it into escaping H and oxidizing O (affecting surface minerals)
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How long is a year, rotation period and day on Venus? začněte se učit
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Year - 225 days, rotation period - 243 days, retrograde, day - 117 days
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What did Pioneer discover about hydrogen isotopes on Venus and what is the interpretation? začněte se učit
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D/H ratio 100× as big as on Earth. Models suggest it could be explained by a presence of ocean in the first 2 Gyr which then quickly evaporated
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Why does photodissociation of water vapor not occur on Earth? začněte se učit
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Temperature gradient in the stratosphere leads to vapor condensation in it's lowest part (10-35 km high), preventing it from reaching ionosphere (> 50 km) where the sunlight would have such an effect
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How did the runaway greenhouse effect happen on Venus and could it happen on Earth? začněte se učit
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As the ocean was evaporating and the water vapor was subject to photodissociation, there was a positive feedback loop between temperature on Venus and capacity for vapor in the atmosphere. It will happen in ~2Gyr on Earth once the Sun shines 40% stronger
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Main highland regions on Venus začněte se učit
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Ishtar Terra (northern polar area), Lada Terra (southern polar area), Aphrodite Terra and Beta Regio (closer to equator)
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Composition of venusian surface začněte se učit
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Lowlands (80%) are basaltic, as we know from measurements made by Venera & Vega landers. Highlands (a k a tesserae) are likely more felsic (based on nighttime IR radiation, but no direct measurement yet)
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začněte se učit
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There is no global plate tectonism similar to that on Earth, otherwise the hypsometric distribution wouldn't be unimodal. But there are some localized compressional (wrinkle ridges in the lowlands) and extensional (rifts, e g in Beta Regio) areas
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What is the proposed formation scenario for venusian coronae? začněte se učit
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Uplift from a plume, then collapse of the central part, flattening of the rim
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What can be said about crater count dating of the venusian surface? začněte se učit
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The distribution appears to be completely random, the entire planet's surface send to be similarly aged (estimated at ~0.5 Gyr)
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What is a lower bound on impact crater dimensions on Venus? začněte se učit
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Around 1 km, because of atmospheric screening (small impactors wouldn't make it to the surface)
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Interpretation of pancake domes on Venus začněte se učit
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Volcanic eruptions of high viscosity lava, flattened due to atmospheric pressure
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Categories of channels on Venus začněte se učit
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Lava channels (straight, with levees), sinuous rilles (tight meanders, low viscosity lava erosion), canali (fluvial like, with meanders and point bars, typically found in lowlands), outflow channel Kallistos Vallis, valley networks (maybe lava sapping)
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Describe the largest known channel in the Solar System začněte se učit
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Baltis Vallis, close to 7000 km, canali type channel on Venus, must be old as it's topographic profile indicates heavy tectonic deformation
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Ideas about canali type channel formation on Venus začněte se učit
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Basaltic, alkaline, or ultramafic lava; carbonatite lava (supported by high CO_2 fugacity); turbidity currents but under the atmosphere and not a sea)
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What kind of lava is hypothesized to have carved venusian sinuous rilles? začněte se učit
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Unpolymerized sulfuric or komatiite (high MgO content and erosional capacity), as they can have low viscosities comparable to water
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začněte se učit
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Wind streaks, transverse dunes
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Ideas about tesserae regions on Venus začněte se učit
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They might be old, bearing traces of fluvial erosion, subsequent to which they were tectonically deformed and partially filled with lava
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začněte se učit
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From Earth-based observations we know there is PH_3 (phosphine) in the atmosphere, at the level of ~20 ppb, it could be a biomarker (produced biogenically on Earth), missions to further study atmosphere needed
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Catastrophic model for the resurfacing of Venus začněte se učit
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The viscous mantle losing water and building up heat until it becomes molten and global volcanism takes place, could occur in a cyclic manner
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Equilibrium model for the resurfacing of Venus začněte se učit
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Localized volcanism and resurfacing ongoing. This is supported by observations of high emissivity (emissivity drops quickly with oxidation time) volcanoes surrounded by young tectonic features, also by SO_2 fluctuations in the atmosphere
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How was volcanism on Io first discovered? začněte se učit
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A plume spotted on Voyager navigation images
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Io density and composition začněte se učit
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3.55 g/cm^3 (similar to lunar density of 3.34 g/cm^3), interpreted as iron core and light silicate mantle
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začněte se učit
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Large activity due to tidal heating, enhanced by eccentric orbit and 4-2-1 resonance with Europa and Ganymede. Primarily sulfuric volcanism which gives the moon its yellowish color. Also some silicate volcanism.
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What do we expect about the ocean under the ice on Europa? začněte se učit
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Based on density (3.01 g/cm^3) we expect ~15% water content and ice crust to be 10-30 km thick depending on the model (end member models are thin conductive and thick convective ice layer). NASA Europa Clipper should reach the ocean with radar
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začněte se učit
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Dilation bands, ridges, chaos regions (maybe linked to water plumes)
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Which moons in the Solar System are larger than Mercury? začněte se učit
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Densities of Ganymede and Callisto začněte se učit
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1.93 & 1.83 g/cm^3, therefore 50-70 % water content, thick ice crusts
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Summarize the theory about the expansion of Ganymede začněte se učit
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Dark terrains appear to be cross-cut by younger (also based on crater counting,) bright terrains. An extensional event might have been due to tetragonal ice (which is denser than liquid water) having existed below the ocean and molten
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Types of grooves on Ganymede začněte se učit
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Tilt blocks (with listric faults, spreading center type) and horst&graben (crustal rifts)
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začněte se učit
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Ancient craters preserved as brighter spots on Ganymede's dark areas
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začněte se učit
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Either rising from the center, from the core-mantle boundary, forming a subsurface ocean or a sponge-like collection of pockets in the mantle
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Titan atmosphere composition začněte se učit
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What do we know about lakes on Titan? začněte se učit
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They were hypothesized based on methane in the atmosphere and confirmed with Cassini radar images, found mostly in polar (particularly northern) areas. Liquid hydrocarbons, coming from haze particles dropping from atmosphere ("hydrological" cycle)
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What is the temperature profile of Titan's atmosphere? začněte se učit
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94 K at the surface, decreasing to 70 K up to 40 km high, then increasing again (similarly to Earth's atmosphere profile)
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Why is the presence of methane in the Titan's atmosphere difficult to explain and what's the proposed explanation? začněte se učit
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It should be unstable (~30 Myr). Therefore, it must be continuously replenished. A hydrocarbon ocean had been proposed, but lakes discovered by Cassini are too small. There must be more underground maybe trapped in clathrate and released by cryovolcanism
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Was the hydro(carbon) sphere of Titan the same in the past? začněte se učit
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Some lakes and rivers dried out but the landforms (and rounded cobbles transported by fluvial action) are preserved, particularly at equatorial and northern regions
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Describe eolian process on Titan začněte se učit
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Dunes, particularly fields of longitudinal dunes, have been found. They cover ~20% of the surface. The sediment is likely ice grains which have a different dynamic than sand on Earth
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What's special about the planned landing site of the Dragonfly mission? začněte se učit
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It will explore ejecta of a nearby crater, which can be excavated subsurface material
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What can be said about Titan's interior? začněte se učit
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Given the 1.88 g/cm^3 density, it should have some ice and inner ocean layers, similar to Europa or Ganymede
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Describe the plumes on Enceladus začněte se učit
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They are coming from a specific area - bluish Tiger Stripes on the southern hemisphere. They contain some liquid and gas, salt, hydrogen coming from deep within (core).
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Theories about Enceladus's internal ocean based on heterogeneity of plume sources začněte se učit
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Either the ocean is regional, as only a section of ice layer melted due to tidal heating, or maybe it is global but the thickness of ice crust is varied.
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Orbital mechanics of Triton začněte se učit
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It has retrograde rotation, it's tidally locked, it might have had a more elliptical orbit and Io like past
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Characteristic landforms on Triton začněte se učit
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Cantaloupe terrain, which may be due to cryovolcanism
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Describe geysers on Triton začněte se učit
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Plumes with nitrogen reaching 8 km high, maybe linked to a nitrogen atmosphere
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Main categories of asteroids in terms of composition začněte se učit
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S - silicate, C - carbonaceous, M - metallic
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What is the difference between a dwarf planet and a planet? začněte se učit
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A planet must clear it's orbital surroundings from other bodies
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Characteristic features on the surface of Ceres začněte se učit
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Cryovolcanism, mass wasting, bright salt deposits in craters
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Other bodies besides Jovian and Saturn moons that are expected to have a lot of subsurface water začněte se učit
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What was the heat source for volcanism on Vesta? začněte se učit
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Radiogenic decay of ^26 Al
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Describe the concept of rubble pile asteroids začněte se učit
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Bodies like Itokawa, Ryggu etc. have low density, comparable to icy moons, but it is not because of water but because of very high porosity. They are loosely held together and would fall apart if they spun too fast (e g Dimorphos detached from Didymos)
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What determines the shape of asteroids such as Ryggu, Didymos, Bennu? začněte se učit
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A net product of gravity and centrifugal force, which can be comparably big. Typically results in an equatorial bulge
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What has been found in Ryggu samples? začněte se učit
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Organic molecules, including aminoacids
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začněte se učit
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Scientifically important boulder - larger than 1% of the size of the hosting asteroid
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Describe the redder areas on Ryggu začněte se učit
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They are near the equator due to solar exposure, likely the asteroid used to be closer to the Sun. Mid-latitude-level stripes were formed by mass wasting
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What has already been discovered by the Lucey mission and what's coming? začněte se učit
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It's a NASA mission launched in 2021 which will visit many Jupiter Trojan asteroids. It already visited Dinkinesh and Salem, which is a binary, and discovered that Salem is a contact binary by itself
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What will the Psyche mission be looking for? začněte se učit
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Evidence of ferrolcanism, the answer whether the composition of Psyche is pure metal or metal & silica mix, perspectives for space mining (rare elements like iridium)
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Describe the atmosphere on Pluto začněte se učit
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Tenuous (10 μbar), composed of nitrogen, methane, carbon monoxide
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Upcoming missions to Venus začněte se učit
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NASA: Veritas - new radar map at higher resolution, Da Vinci - atmosphere probing and landing on Tesserae to measure it's composition directly for the first time. ESA: EnVision - studying the climate and such to understand better the difference with Earth
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Is Pluto always further from the Sun than Neptune? začněte se učit
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No, the elliptical orbit is partially inside, e g 1979-1999
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What are the dunes on Pluto composed of and how is the sediment transported? začněte se učit
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200-300 μm methane ice particles. The winds at Pluto are strong enough to sustain their transport but not to initiate it, so maybe they form by sublimation in the atmosphere
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Characteristic feature on Charon začněte se učit
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A large graben-like trough
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What other trans-Neptunian object was visited by New Horizons and what did we learn about it? začněte se učit
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A contact binary Arrokoth, composed of two spherules: 19 km Ultima and 14 km Thule. It is similar to the 67P comet and in fact that comet came from the Kuiper Belt
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What do we know about comet composition? začněte se učit
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They are dirty snowballs, composed of volatiles (H_2O, CO_2, CO...), silicates and some organic compounds
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Parent bodies for Orionid and Geminid meteor showers začněte se učit
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Halley's comet and Phaeton, respectively
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