deglaciation वाक्य
उदाहरण वाक्य
मोबाइल
- Periods of deglaciation are also caused in part by oceanic processes.
- However, during deglaciation, the faults experience accelerated slip triggering earthquakes.
- The total uplift from the end of deglaciation may be up to.
- Germany's alpine glaciers are experiencing deglaciation.
- The initial uplift following deglaciation was almost immediate due to the exponentially after that.
- Rapid deglaciation occurred after the disappearance of Lake Tauca 14, 000 years ago.
- Some believe this story describes the environment of the Northwest Coast during the last deglaciation.
- Today, more than 6000 years after the last deglaciation terminated, the flow of oblate.
- The deglaciation patterns of the Bergen and Nordfjord Sunnm�re areas in western Norway are described and correlated.
- Once deglaciation was complete, uplift slowed to about annually, and it decreased exponentially after that.
- Magma probably formed during deglaciation was erupted during the early Holocene, generating the long lava flow.
- During deglaciation, the melted ice-water returned to the oceans, causing sea level to rise.
- Beginning with the Lic�n Ignimbrite, generated just after the last deglaciation, activity continued in similar fashion.
- If present deglaciation trends continue, the Calderone may soon share Corral de la Veleta's fate.
- Oxygen isotope values from high latitudes : clues for Permian sea-surface temperature gradients and Late Paleozoic deglaciation.
- The lands of Novaya Zemlya attained most of their early Holocene coastal deglaciation approximately 10, 000 years before present.
- During deglaciation, the melted ice water returns to the oceans, thus sea level in the ocean increases again.
- In the Alps this maximum was in 1850 and since then the region has become ice free due to deglaciation.
- After deglaciation, snow and ice melt from the mountain tops can create streams and rivers in U-shaped valleys.
- The physical mechanisms by which deglaciation occurs include melting, evaporation, calving, and aeolian processes such as wind scouring.
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