lobated การใช้
- When opposing lobate debris aprons converge, linear valley fill results.
- Lobate scarps are the most common structural landforms in the Bach region.
- These glaciers are termed lobate debris aprons when surrounding mounds and mesas.
- However the relationship of smooth and lobate plains is uncertain.
- Like lobate debris aprons, they are believed to be ice-rich.
- These deposits of rock debris are called lobate debris aprons ( LDAs ).
- Its structure is massive and lobate, with lobe diameters expanding downflow from.
- The sponge mass is lobated, with regular to irregularly shaped lobes typically tall.
- It has an outer lobate ejecta deposit extending about a crater radius from the rim.
- The lobate and has a distinct neck.
- These glaciers are termed lobate debris aprons ( LDA ) when surrounding mounds and mesas.
- In addition, lobate debris aprons can show surface lineations just as rock glaciers on the Earth.
- On the floor is a lobate scarp that was formed as a result of contraction of the lava.
- Image : Lobate feature with hiwish . JPG | Probable glacier as seen by HiRISE under HiWish program.
- The distinctive lobate ejecta pattern of craters like Yuty gave rise to a confusing terminology among Mars researchers.
- Grain boundaries are lobate with a variable grain size, with new grains generally larger than existing subgrains.
- Rembrandt basin is cross-cut by a large lobate scarp running from the southwest to the north.
- This plant does indeed have a variety of leaf forms, with only the larger leaves being lobate.
- The volcanic field is dominated by a plateau made of lobate lava flows, typically having thicknesses of.
- At very high temperatures, grains are highly lobate or ameboid, but can be nearly strain-free.
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