Pasang Steam
sign in
|
bahasa
简体中文 (Bahasa Cina Dipermudah)
繁體中文 (Bahasa Cina Tradisional)
日本語 (Bahasa Jepun)
한국어 (Bahasa Korea)
ไทย (Bahasa Thai)
Bahasa Indonesia
Български (Bahasa Bulgaria)
Čeština (Bahasa Czech)
Dansk (Bahasa Denmark)
Deutsch (Bahasa Jerman)
English (Bahasa Inggeris)
Español – España (Bahasa Sepanyol – Sepanyol)
Español – Latinoamérica (Bahasa Sepanyol – Amerika Latin)
Ελληνικά (Bahasa Greek)
Français (Bahasa Perancis)
Italiano (Bahasa Itali)
Magyar (Bahasa Hungary)
Nederlands (Bahasa Belanda)
Norsk (Bahasa Norway)
Polski (Bahasa Poland)
Português (Bahasa Portugis – Portugal)
Português – Brasil (Bahasa Portugis – Brazil)
Română (Bahasa Romania)
Русский (Bahasa Rusia)
Suomi (Bahasa Finland)
Svenska (Bahasa Sweden)
Türkçe (Bahasa Turkiye)
Tiếng Việt (Bahasa Vietnam)
Українська (Bahasa Ukraine)
Laporkan masalah terjemahan

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
⠀⠀⠀⠀ ⠀⣠⣴⠶⠷⠶⣦⡀⠀⠀⠀⣀⣴⠶⠿⣶⣦⣀
⠀⠀⠀⠀⢀⣾⡟⠁⠀⠀⠀⠀⠙⣦⢀⡼⠋⠀⣀⠀⠀⠙⠻⣦
⠀⠀⠀⠀⣼⡟⠀⠀⠀⠀⠀⠀⠀⠈⠟⠀⢀⣿⣿⣇⠀⠀⢀⠙⠆
⠀⠀⠀⠀⣿⠃⠀⠀⠀⠀⠀⠀⠀⣠⣄⠀⢸⣿⣿⡿⢠⣾⣿⣷
⠀⠀⠀⠀⣿⡀⠀⠀⠀⠀⠀⠀⢸⣿⣿⣇⠸⣿⣿⠃⣿⣿⣿⡟
⠀⠀⠀⠀⠸⣧⠀⠀⠀⠀⠀⠀⢸⣿⣿⡟⠀⠀⠀⠀⠿⠿⠟⣀⣀
⠀⠀⠀⠀⠀⠙⢷⣄⠀⠀⠀⠀⠀⠙⣋⣤⣶⣾⣷⣦⠀⣠⣿⣿⣿⡆
⠀⠀⠀⠀⠀⠀⠀⠙⢷⣄⠀⠀⠀⣾⣿⣿⣿⣿⣿⣿⡆⣿⣿⣿⡿⠁
⠀⠀⠀⠀⠀⠀⠀⠀⠀⠉⠻⣦⡈⣿⣿⣿⣿⣿⣿⣿⣿⠈⠉⠉
⠀⠀⠀⠀⠀⠀⠀⠀⠀⠀⠀⠈⢿⣎⠛⣛⢿⣿⣿⣿⣿
⠀⠀⠀⠀⠀⠀⠀⠀⠀⠀⠀⠀⠀⠹⣿⠏⠀⠉⠻⠿⠋