walther's law Flashcards
(12 cards)
state Walther’s law and explain its significance in sedimentary geology (3)
- “facies that occur in conformable vertical successions also occurred in laterally adjacent environments”
- significant in interpreting past depositional environments
- linking vertical changes to horizontal shifts due to sea-level change or migration of environments
describe how Walther’s law can help interpret a transgressive sequence (4)
- a transgression involves sea level rising
- environments shifting landward
- vertical facies succession from coarse to fine
- deeper water facies overlie shallower water facies due to landward shift
using Walther’s law, describe how a vertical succession of sedimentary rocks might form during regression (4)
- regression is sea level falling
- environments shift seaward
- vertical sequence from deeper to shallower
- seaward migration of depositional environments
what are the limitations of using Walther’s law when interpreting sedimentary sequences (3)
- not applying across unconformities or where deposition is interrupted
- assuming lateral continuity that may not exist
- challenges when tectonics or erosion complicate facies relationships
compare how Walther’s law can be applied to both shallow marine and fluvial environments (4)
- shallow marine facies migrating landward or seaward due to sea-level changes
- fluvial environments shifting laterally due to channel migration
- both showing vertical facies changes reflecting lateral environmental shifts
- (differences) marine more affected by sea level; fluvial by sediment supply and gradient
explain how Walther’s law helps geologists understand past environmental changes (3)
- linking vertical facies changes to lateral migration
- reconstructing sequences of depositional environments
- recognising events like transgressions or regressions
describe how a transgressive-regressive cycle would appear in a vertical sequence, according to Walther’s law (4)
- transgression: deeper facies over shallower
- regression: shallower facies over deeper
- symmetrical or stacked pattern in rock record
- interpreting sea-level change from these vertical successions
what conditions must be met for Walther’s law to be valid (3)
- conformable deposition (no significant breaks/unconformities)
- continuous lateral migration of environments
- facies being genetically related and part of the same depositional system
explain how Walther’s law can aid in the correlation of sedimentary sequences between outcrops (4)
- using vertical facies patterns to infer lateral continuity
- identifying similar sequences in different locations
- matching transgressive/regressive trends
- reconstructing paleogeography and depositional environments
marine transgression
a geological event during which SEA LEVEL RISES relative to the land and the shoreline moves toward higher ground
marine regression
a geological process occurring when areas of submerged seafloor are exposed above the sea level — SEA LEVEL FALLING
Walther’s law states:
“the vertical succession of facies reflects lateral changes in environment”
in other words, environments that are next to each other in space will appear one above the other in a vertical sequence of strata, provided there is no significant break in sedimentation (i.e. no unconformity)
key concepts:
- facies: a facies is a body of rock with specific characteristics — such as grain size, composition, or fossil content — that reflect a particular depositional environment (e.g. beach, lagoon, reef)
- lateral to vertical transition: as depositional environments shift (due to sea-level change), the sediments deposited in one environment will be over lain by those from another. what was once a beach might be overlain by offshore mud as sea level rises
- continuous deposition: Walther’s law only applies when deposition is uninterrupted (no erosion or long breaks in time)
example:
let’s say a shoreline moves inland due to sea level rise (a transgression). the following vertical sequence may develop:
top offshore mud (deep marine facies)
————————————————————————————
middle shoreface sand (beach facies)
————————————————————————————
bottom coastal marsh mud (tidal flat)
these environments were originally side-by-side. as sea level rose, each moved landward, stacking their sediments vertically over time
…