levo

Dryland Landscapes

Rock type and structure in dryland landscapes

  • 3 things to know
  • Component 01

Overview

Recall questions on lithology and rock resistance in deserts, mesas and buttes in Monument Valley, permeability, joints and bedding planes, calcrete, gypcrete and silcrete duricrusts, sandstone as a dune source, dipping strata, and faulting in the Basin and Range Province.

What you need to know

Answer each one before you reveal it.

Your recallNot started
Key term

Define lithology as a control on dryland landforms

Key term

Why do horizontally bedded resistant strata produce mesas and buttes?

Key term

Name a desert landscape famous for mesas and buttes cut in horizontal sandstone.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Define the term lithology.

    Model answer

    Lithology is the physical and chemical character of a rock, including its mineral composition, grain size, hardness and permeability.

  2. 2

    How does rock resistance control the shape of a desert slope?

    Model answer

    Resistant beds stand out as vertical cliffs and caprocks while weaker beds are worn back into gentler debris-covered slopes, producing a stepped slope profile.

  3. 3

    Why do horizontally bedded resistant strata produce mesas and buttes?

    Model answer

    A hard caprock protects the weaker rock beneath it, so the plateau can only retreat by undercutting and collapse at its edges, leaving flat-topped remnants that shrink into isolated buttes.

  4. 4

    Name a desert landscape famous for mesas and buttes cut in horizontal sandstone.

    Model answer

    Monument Valley, on the Colorado Plateau of the south-western United States, is famous for its mesas and buttes.

  5. 5

    How does permeability influence runoff in a desert?

    Model answer

    Permeable rocks such as jointed sandstone and limestone absorb what little rain falls so surface channels are rare, while impermeable shale and clay shed water and develop dense gully networks.

  6. 6

    Why are joints and bedding planes so important in desert weathering?

    Model answer

    They are lines of weakness along which water, salts and roots can penetrate the rock, so weathering attacks inwards from them and progressively loosens individual blocks.

Other ways to work this

The same content, four other ways.

What is inside Levo

Six ways to work the same material.

1Closed book
2Open book
3Closed book

The 3-step method, run for you

Answer cold, learn it, then prove it stuck. Levo tracks the jump between your first attempt and your last.

Coastal Landscapes
Glaciated Landscapes
Dryland Landscapes
Earth’s Life Support Systems

Cram a whole paper in one sitting

Sort every topic into what you know and what you do not, then drill only the weak ones.

Hotter magma is .
runnierthickerslower

Blank Blitz makes facts automatic

Rapid timed gap-fills on the terms and numbers you need to recall without thinking.

AThe lower quartile is the 2nd value, 11 cm.
BThe upper quartile is the 6th value, 16 cm.
CThe interquartile range is 16 − 11 = 5 cm.

Build It gets the exam shape right

Assemble a full-mark answer from its marking points, in the order an examiner wants them.

The sunspot cycle lasts about 11 years.
TrueFalse

Test It catches misconceptions

Spot the fault in a statement. The traps are the mistakes students actually make.

721941163128510

Brain Breaks between sessions

Short focus games to reset attention, so the next set lands better than the last.

Every question in Dryland Landscapes, on a schedule.

Attempt a question from memory, write the correct version, then attempt it again. Levo records the jump between your first attempt and your last, and brings each question back on the day you are due to forget it.

Or £46 a year, about £3.83 a month. Cancel anytime.