SEAFLOOR-SPREADING
Sea Floor Spreading
Introduction
Proposed by American geophysicist Harry Hammond Hess in 1960.
Utilizes SONAR (Sound Navigation And Ranging) to map the ocean floor.
SONAR Technology
SONAR sends pulses of sound waves through water.
Waves reflect back when hitting objects (e.g., fish, vegetation, seafloor).
The device measures the time taken for the echo to return.
Echolocation
Example: Insect-eating bats rely on echolocation due to blindness in darkness.
Counterpart: Flying Fox or Giant Fruit-eating Bat also uses echolocation.
Mid-Oceanic Ridge
Characterized by "stretched marks" on the seafloor where water is drained.
Consists of underwater mountain ranges.
Mechanism of Sea Floor Spreading
Occurs at mid-ocean ridges due to the upward movement of magma.
Convection currents push magma upward, which liquefies and transforms surrounding rocks.
When magma reaches the surface, it cools and pushes older rocks outward, similar to magnetic fields.
New Oceanic Crust Formation
Younger materials form new oceanic crust, contributing to the ocean floor's expansion.
This process is believed to occur every 200 million years.
Evidence Supporting Sea Floor Spreading Theory
Magnetic Strips: Rocks exhibit patterns of magnetic orientation.
Spinning Core: Core's magnetic orientation changes approximately every 2,000 years, captured by newly formed rocks.
Radiometric Age: Ocean floor rocks are significantly younger than continental crust rocks.
Seafloor Drill Data: Different ages and densities of rocks found in layers substantiate the theory.
Molten Material Evidence: Rock formations resemble shapes created by toothpaste, indicating molten eruptions.
Quiz Questions
What is the mid-ocean ridge?
c. Mountain chains on the ocean floor.
Evidence supporting age differences in oceanic crust?
c. The radiometric age of the two layers of oceanic crust.
Proposer of seafloor spreading theory?
b. Harry Hess.
True or False: Rocks under the ocean floor align with magnetic lines?
a. true.
Why does the seafloor spread?
a. Due to the upward movement of molten materials leading to new oceanic crust formation.