Mr. Crabs lives in a gray anchor under the sea, but his mom also lives in a pink anchor under the sea.
Address: Under the sea, next to squidward and about 3 yards away from the krusty krab
Yup! They're beautiful!
Spongebob squarepants.
i only know one twenty thousand leagues under the sea starring James masonMore Sea Stories30000 Leagues under the Sea (2007) Beyond the Sea (2004) the story of Bobby DarinThe Sea Inside or "Mar Adentro" 2004The Salton Sea 2002 Val KilmerSea (2001)Sea of Love (1989) Al PacinoDeep Blue Sea (1999) Thomas JaneAround the World Under the Sea (1966) Lloyd BridgesThe Sunshine Sea -- a re-make of "Waves of Change" 1970Doctor at Sea (1955) Dirk BogardeAmerican Sea Power (1941 war documentary)The Sea Hawk 1940
yes, they can
Folding and faulting in Earth's crust are typically caused by the deformation of rocks under pressure. Rocks that commonly fold include sedimentary rocks like shale and sandstone, while faulting can occur in any type of rock. The materials involved in the process are the rocks themselves, along with pressure from tectonic forces and heat from the Earth's interior.
Yes, it is quite common for earthquakes to occur under the sea. But they can also occur under the land. Any location on the Earth's surface (or close to the Earth's surface, to be more accurate) can have an earthquake, although of course, some locations are more prone to earthquakes than others.
An earthquake occurred under the pacific sea floor.
cause japan is under sea level.
at boundaries between moving parts of the crust
At interfaces between moving parts of the lithosphere
tsunamis usually occurs after an earthquake specially under sea earthquakes.
Normal faulting, where the hanging wall moves downward relative to the footwall. Reverse faulting, where the hanging wall moves upward relative to the footwall. Strike-slip faulting, where horizontal movement occurs parallel to the fault plane.
Sea floor spreading
EARTHQUAKES - the sudden, intense shift along already formed fault cause earthquake to occur -earthquake occur around plate boundary where plate movement occur in the form of faulting
Three mechanisms for crustal thickening are magmatic intrusion, sedimentation, and faulting.