The slope of the internal zone typically refers to the gradient or steepness of a specific area within a larger system, such as a geological formation or an economic model. In geological terms, it can indicate how quickly elevation changes occur within a certain region, while in economic contexts, it may relate to the relationship between variables like supply and demand within a market. The specific value of the slope would depend on the context and the data being analyzed.
then the slope is x=y. there is no slope.
Examples of slope: http://www.answers.com/topic/slope http://en.wikipedia.org/wiki/Slope
Yes, it is true; slope zero is no slope.
The continental slope is crucial for several reasons. It serves as a transitional zone between the shallow waters of the continental shelf and the deep ocean, playing a key role in marine ecosystems and biodiversity. Additionally, it is rich in resources such as oil, gas, and minerals, making it significant for economic activities like fishing and energy exploration. Furthermore, the slope influences ocean currents and sediment transport, impacting climate and marine life.
X=5 is a vertical line, so it has no slope. When I say it has no slope, I don't mean the slope is 0, I mean the slope is nonexistent.
The major internal cause of slope failure is excessive saturation of the soil, leading to loss of strength and increased pore water pressure. This can be triggered by factors such as heavy rainfall, poor drainage, or improper construction practices that disturb the natural slope stability.
continental slope
Same area: Lower part is continental shelf whereas the upper part is exclusive economic zone. Seabed or Subsoil is covered in continental shelf whereas above that is exclusive economic zone.
The abyssal zone is not included in the continental margin. It is the deep ocean floor beyond the continental shelf, slope, and rise.
The zone between the continental shelf and the abyssal zone is known as the continental slope. This area features a steep decline from the continental shelf, transitioning into deeper ocean waters. It typically ranges from depths of about 200 meters to around 3,000 meters. The continental slope is characterized by various geological features and is often rich in marine life due to nutrient runoff from the shelf above.
Yes, the internal zone, often referred to as the benthic zone, includes the bottom of a water body where organisms live on or in the sediment. This zone is characterized by a variety of organisms, including bacteria, worms, mollusks, and crustaceans, that play essential roles in the ecosystem. The benthos is crucial for nutrient cycling and serves as a food source for higher trophic levels.
The ocean zone that covers the continental shelf is called the neritic zone. It extends from the shoreline to the edge of the continental shelf, which is typically around 200 meters deep. This zone is characterized by high levels of sunlight, nutrients, and biodiversity.
The internal zone, often referred to in various contexts such as psychology or ecology, typically describes an area that is protected or insulated from external influences. In psychology, it can relate to an individual's personal space or emotional boundaries. In ecological terms, it may denote a core area within an ecosystem that is less affected by external disturbances. Understanding the internal zone is crucial for maintaining stability and health in both personal well-being and environmental sustainability.
The continental shelf, slope, and rise combine to form the continental margin. The continental shelf is the shallow, submerged extension of a continent, the slope is the steep incline that leads to the ocean floor, and the rise is the gently sloping accumulation of sediment at the base of the slope. Together, they make up the transition zone between the continent and the deep ocean.
The continental shelf, continental slope, and continental rise combine to form the continental margin. The continental margin is the transition zone between the continent and the deep ocean basin.
there is 2 one in iron island(room on left when you enter one in the desert in the battle zone(down a bike slope)
The Sun's internal structure consists of several layers, primarily the core, radiative zone, and convective zone. The core, where nuclear fusion occurs, generates energy and is extremely hot and dense. Surrounding the core is the radiative zone, where energy is transferred outward through radiation, and above that is the convective zone, where energy is transported by convection currents. This layered structure plays a crucial role in the Sun's energy production and overall dynamics.