- published: 04 Apr 2013
- views: 11973
The seabed (also known as the seafloor, sea floor, or ocean floor) is the bottom of the ocean.
Most of the oceans have a common structure, created by common physical phenomena, mainly from tectonic movement, and sediment from various sources. The structure of the oceans, starting with the continents, begins usually with a continental shelf, continues to the continental slope – which is a steep descent into the ocean, until reaching the abyssal plain – a topographic plain, the beginning of the seabed, and its main area. The border between the continental slope and the abyssal plain usually has a more gradual descent, and is called the continental rise, which is caused by sediment cascading down the continental slope.
The mid-ocean ridge, as its name implies, is a mountainous rise through the middle of all the oceans, between the continents. Typically a rift runs along the edge of this ridge. Along tectonic plate edges there are typically oceanic trenches – deep valleys, created by the mantle circulation movement from the mid-ocean mountain ridge to the oceanic trench.
"Soul and Fire" by Sebadoh
Written by Lou Barlow
from _Bubble and Scrape_
It's all a matter
of soul and fire.
Infatuation
or true desire.
The thrill of discovery,
divine intervention;
cruel, cruel change,
pain of rejection.
As you walk away
think of all the joy we shared.
If you decide you need me,
I'll be wondering if I care...
Not there to soothe your soul,
friend to tender friend.
I think our love is coming to an end.
King persuader,
congratulations.
You share her heart,
you bought her soul
Princess confusion
come to me again.
Saying goodbye
was so much fun.
When you walk away
feel the freedom in your heart.
There's a joy in letting go,
free to find a love apart.
When I lose control
I need a kind, forgiving friend,
but I think our love is coming to an end.