Sandstone, mudstone, fossiliferous/oolitic limestone, sand ridges, and tempestites are all possible features of the continental shelf, which is a progression in grain size away from the coast. commonly known as the passive margin, a large, shallow region.
What precisely is the continental shelf?Geologists typically refer to the area of the continental margin that is located between the shoreline and the shelf break or, in the absence of a discernible slope, between the shoreline and the location where the depth of the water immediately adjacent to the shore is approximately between 100 and 200 meters.
What is the continental shelf, and why is it important?A continent's oceanic edge is referred to as its continental shelf. The seven primary geographic divisions on Earth are known as continents. A continental shelf extends from the shoreline of a continent to a point where it drops off, which is referred to as the shelf break.
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Sandstone, mudstone, fossiliferous/oolitic limestone, sand ridges, and tempestites are all possible features of the continental shelf, which is a progression in grain size away from the coast. commonly known as the passive margin, a large, shallow region.
What precisely is the continental shelf?Geologists typically refer to the area of the continental margin that is located between the shoreline and the shelf break or, in the absence of a discernible slope, between the shoreline and the location where the depth of the water immediately adjacent to the shore is approximately between 100 and 200 meters.
What is the continental shelf, and why is it important?A continent's oceanic edge is referred to as its continental shelf. The seven primary geographic divisions on Earth are known as continents. A continental shelf extends from the shoreline of a continent to a point where it drops off, which is referred to as the shelf break.
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Human activities that have contributed to shoreline erosion include:
a. seasonal traffic at beaches during the summer months
b. depositional processes
c. placement of seawalls along the shoreline
d. excess fishing and boating activities
Answer:
I think the answer is c. placement of seawalls along the shoreline
Explanation:
Human activities that have contributed to shoreline erosion include: seasonal traffic at beaches during the summer months; depositional processes; the placement of seawalls along the shoreline; and excessive fishing and boating activities.
a. Seasonal traffic at beaches during the summer months can result in the removal of sand and vegetation, which can contribute to shoreline erosion. b. Depositional processes such as sand mining and dredging can lead to a lack of sediment supply to the beach, resulting in shoreline erosion. c. The placement of seawalls along the shoreline can contribute to shoreline erosion by disrupting natural sediment transport processes and altering wave energy. d. Excess fishing and boating activities can lead to the destruction of shoreline vegetation, which can result in increased erosion. Additionally, the disturbance of sediment by boats and anchors can contribute to shoreline erosion.
It's important to note that option b, depositional processes, is not a human activity and is actually a natural process that can help counteract erosion by adding sediment to the shoreline.
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why would one conclude that high stream order in a valley network would be more characteristic of rainfall runoff than groundwater sapping?
High stream order in a valley network is more characteristic of rainfall runoff than groundwater sapping: because rainfall runoff generates larger volumes of water
First, rainfall runoff is the process by which excess water from rain, snowmelt, or other sources flows over the land surface. This results in a higher stream order, as larger volumes of water contribute to the formation and growth of river systems.
This increased water volume and flow velocity lead to the erosion of valley networks, causing the development of branching patterns.
On the other hand, groundwater sapping is a process in which groundwater slowly erodes the landscape, forming valleys and channels. Groundwater sapping typically results in lower stream orders, as the process is slower and does not generate as much flow as rainfall runoff.
Additionally, rainfall runoff usually occurs more rapidly, leading to a higher likelihood of flash floods and the creation of a more extensive network of interconnected streams. Groundwater sapping, being a slower process, tends to form less extensive networks with lower stream orders.
In summary, high stream order in a valley network is more characteristic of rainfall runoff than groundwater sapping because rainfall runoff generates larger volumes of water, occurs more rapidly, and leads to the development of more extensive and interconnected networks of streams.
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discussion on different types of drought
Explanation:
Drought is a natural disaster that occurs when there is insufficient rainfall for an extended period of time, leading to a shortage of water resources. Different types of drought can occur depending on the region, climatic conditions, and severity of the drought. In this discussion, we will explore some of the different types of droughts.
1. Meteorological drought: This type of drought occurs due to a prolonged period of below-average precipitation, leading to a deficit in soil moisture and reduced water availability. Meteorological droughts are often caused by changes in weather patterns such as El Niño or La Niña.
2. Agricultural drought: This type of drought affects agricultural crops and livestock, and occurs when there is a deficiency of soil moisture or inadequate rainfall during the growing season. It can lead to crop failure, loss of livestock, and reduced yields. Agricultural droughts can have significant economic impacts on farming communities and food prices.
3. Hydrological drought: This type of drought is caused by a deficit of water in rivers, lakes, and groundwater sources. Hydrological droughts can result from a combination of reduced precipitation and increased water usage. They can have far-reaching impacts on ecosystems, habitats, and human societies that depend on these water sources.
4. Socioeconomic drought: This type of drought encompasses the social and economic impacts of drought, which can include increased unemployment, loss of income, and food insecurity. Socioeconomic droughts have a disproportionate impact on vulnerable populations, particularly those living in poverty, and can exacerbate existing inequalities.
5. Ecological drought: This type of drought affects ecosystems, biodiversity, and natural resources, leading to damage to plant and animal species and their habitats. Ecological droughts can be caused by a lack of water, changes in temperature, and other factors.
In conclusion, understanding the different types of drought is important for predicting and managing their impacts. Effective drought management strategies may include water conservation, drought-resistant crop varieties, and early warning systems.
Which of the following environmental problems is most directly linked to ocean warming?
A
Coral bleaching
B
Beaching of whales and dolphins
C
Decreased global sea level
D
Decreased ocean sedimentation
which of these numbered features contains most of earth’s freshwater? lakes groundwater glaciers and ice sheets atmosphere ocean
The feature that contains most of Earth's freshwater is glaciers and ice sheets.
Glaciers and ice sheets hold about 68.7% of Earth's freshwater, while groundwater accounts for about 30.1%. Lakes, rivers, and swamps hold only about 0.3% of Earth's freshwater. The atmosphere holds only a small amount of freshwater, mostly in the form of water vapor. The ocean holds the largest volume of water on Earth, but it is saline, with only about 2.5% of it being freshwater.
The importance of glaciers and ice sheets as freshwater reservoirs cannot be overstated. They act as "frozen reservoirs" that store freshwater as snow and ice, releasing it slowly over time, which helps regulate the flow of freshwater to streams and rivers. The melting of glaciers and ice sheets due to climate change can have profound impacts on freshwater availability and can cause changes in water availability and quality, affecting human populations, ecosystems, and economies.
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