Nainstalovat Steam
přihlásit se
|
jazyk
简体中文 (Zjednodušená čínština)
繁體中文 (Tradiční čínština)
日本語 (Japonština)
한국어 (Korejština)
ไทย (Thajština)
български (Bulharština)
Dansk (Dánština)
Deutsch (Němčina)
English (Angličtina)
Español-España (Evropská španělština)
Español-Latinoamérica (Latin. španělština)
Ελληνικά (Řečtina)
Français (Francouzština)
Italiano (Italština)
Bahasa Indonesia (Indonéština)
Magyar (Maďarština)
Nederlands (Nizozemština)
Norsk (Norština)
Polski (Polština)
Português (Evropská portugalština)
Português-Brasil (Brazilská portugalština)
Română (Rumunština)
Русский (Ruština)
Suomi (Finština)
Svenska (Švédština)
Türkçe (Turečtina)
Tiếng Việt (Vietnamština)
Українська (Ukrajinština)
Nahlásit problém s překladem

Texas, United States



Typical rift features are a central linear downfaulted segment, called a graben, with parallel normal faulting and rift-flank uplifts on either side forming a rift valley, where the rift remains above sea level. The axis of the rift area commonly contains volcanic rocks and active volcanism is a part of many, but not all active rift systems.
Major rifts occur along the central axis of mid-ocean ridges, where new oceanic crust and lithosphere is created along a divergent boundary between two tectonic plates.
Failed rifts are where continental rifting began, but then failed to continue to the point of break-up. Typically the transition from rifting to spreading develops at a triple junction where three converging rifts meet over a hotspot. Two of these evolve to the point of seafloor spreading, while the third ultimately fails, becoming
⠀⠀⠀⠀ ⠀⣠⣴⠶⠷⠶⣦⡀⠀⠀⠀⣀⣴⠶⠿⣶⣦⣀
⠀⠀⠀⠀⢀⣾⡟⠁⠀⠀⠀⠀⠙⣦⢀⡼⠋⠀⣀⠀⠀⠙⠻⣦
⠀⠀⠀⠀⣼⡟⠀⠀⠀⠀⠀⠀⠀⠈⠟⠀⢀⣿⣿⣇⠀⠀⢀⠙⠆
⠀⠀⠀⠀⣿⠃⠀⠀⠀⠀⠀⠀⠀⣠⣄⠀⢸⣿⣿⡿⢠⣾⣿⣷
⠀⠀⠀⠀⣿⡀⠀⠀⠀⠀⠀⠀⢸⣿⣿⣇⠸⣿⣿⠃⣿⣿⣿⡟
⠀⠀⠀⠀⠸⣧⠀⠀⠀⠀⠀⠀⢸⣿⣿⡟⠀⠀⠀⠀⠿⠿⠟⣀⣀
⠀⠀⠀⠀⠀⠙⢷⣄⠀⠀⠀⠀⠀⠙⣋⣤⣶⣾⣷⣦⠀⣠⣿⣿⣿⡆
⠀⠀⠀⠀⠀⠀⠀⠙⢷⣄⠀⠀⠀⣾⣿⣿⣿⣿⣿⣿⡆⣿⣿⣿⡿⠁
⠀⠀⠀⠀⠀⠀⠀⠀⠀⠉⠻⣦⡈⣿⣿⣿⣿⣿⣿⣿⣿⠈⠉⠉
⠀⠀⠀⠀⠀⠀⠀⠀⠀⠀⠀⠈⢿⣎⠛⣛⢿⣿⣿⣿⣿
⠀⠀⠀⠀⠀⠀⠀⠀⠀⠀⠀⠀⠀⠹⣿⠏⠀⠉⠻⠿⠋