cross-bedding wikipedia - EAS
- In geology, cross-bedding, also known as cross-stratification, is layering within a stratum and at an angle to the main bedding plane. The sedimentary structures which result are roughly horizontal units composed of inclined layers. The original depositional layering is tilted, such tilting not being the result of post-depositional deformation.en.wikipedia.org/wiki/Cross-bedding
- 大家還會問
- 查看更多內容檢視所有 Wikipedia
In geology, cross-bedding, also known as cross-stratification, is layering within a stratum and at an angle to the main bedding plane. The sedimentary structures which result are roughly horizontal units composed of inclined layers. The original depositional layering is tilted, such tilting not being the result … 查看更多內容
Cross-beds can tell geologists much about what an area was like in ancient times. The direction the beds are dipping indicates paleocurrent, the rough direction of sediment transport. The type and condition of sediments … 查看更多內容
Rivers
Flows are characterized by climate (snows, rain, and ice melting) and gradient. Discharge variations measured on a variety of time scales can change water depth, and speed. Some rivers can be … 查看更多內容CC-BY-SA 授權下的維基百科文字 Cross-bedding - Wikipedia
Category:Cross-bedding - Wikipedia
Cross-bedding Wikipedia 的圖片
bing.com/imagesCross-bedding - Wikiwand
Category:Cross-bedding - Wikimedia Commons
Cross-bedding - AAPG Wiki
Cross-bedding | Detailed Pedia
Cross-bedding - AAPG Wiki
Talk:Cross-bedding - Wikipedia
- 部分搜尋結果已被移除