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What else can I help you with?
What is the difference between a cylinder and a cuboid?
A cylinder has a circular cross-section whereas a cuboid has a quadrilateral cross-section.
How do you find the cross section volume of a trapezoid with a change in slope?
The cross section volume of a trapezoid is found between 0 and 2.0.
What is the difference between the cross section of a pyramid and the cross section of a prism?
The cross section of a pyramid shrinks from the shape of the base down to a point as you move along its axis from the base to the apex. The cross section of a prism is constant along its axis.
What is a cross section of a cone?
Circle: If the knife is perpendicular to the axis of the cone.Ellipse: If the knife is between (perpendicular to the axis of the cone) and (parallel to the side of the cone).Parabola: If the knife is between (parallel to the side of the cone) and (parallel to the axis of the cone).Hyperbola: If the knife is parallel to the axis of the cone.Triangle: If the knife is perpendicular to the base of the cone.Point: If the knife is parallel to the base the cone and through the apex
How many angles does a cross have?
A cross has 4 angles
Whats the difference in graded bedding and cross bedding?
Surfaces between layers of sediments (bedding planes) are usually deposited in horizontal sheets, but cross-bedding is inclined. Graded beds are horizontal and are usually sorted from coarse at the bottom to fine at the top.
Is it possible for a layer of cross bedding strata show graded bedding as well?
Absolutely: there are many possibilities. The only issue is that as the cross-bedding is often not on a massive scale, this may cause graded bedding to become unnoticeable. It is clearer in a rock with only graded bedding. As the beds are often quite shallow, grading is often unnoticeable, yet it still may exist on a slight scale.
Is it possible for a layer of cross-bedded strata to show graded bedding as well?
Absolutely: there are many possibilities. The only issue is that as the cross-bedding is often not on a massive scale, this may cause graded bedding to become unnoticeable. It is clearer in a rock with only graded bedding. As the beds are often quite shallow, grading is often unnoticeable, yet it still may exist on a slight scale.
What is planar bedding and cross bedding?
In planer bedding Surfaces are without cross lines, but cross-bedding is inclined.
Compare and contrast graded bedding and cross-bedding?
Cross-Bedding is a feature that occurs at various scales, and is observed in conglomerates and sandstones. It reflects the transport of gravel and sand by currents that flow over the sediment surface (e.g. in a river channel). sand in river channels or coastal environments. Graded Bedding means that the grain size within a bed decreases upwards.
What is the wavy line between layers of rock called?
The wavy line between layers of rock is called a "cross bedding." Cross bedding forms when sediments are deposited at an angle due to currents, resulting in distinct layers that intersect at an angle to the horizontal bedding.
Which features tells you how a sedimentary rock is layered?
The features that indicate how a sedimentary rock is layered include bedding planes, which represent the boundaries between different layers of sediment, and graded bedding, where grains are sorted by size within a layer. Additionally, cross-bedding can show inclined layers within a sedimentary rock, indicating the direction of sediment deposition.
Cross-bedding is a feature of?
Deltas
Distinguish between f1 generation and f2 generation?
The F1 generation consists of the offspring of a cross between two parents; the F2 generation consists of the offspring of a cross between two individuals in the same F1 generation.
Cross-bedding is a feature of and sand dunes?
deltas
What is the type of bedding that occurs depends upon the sediments method?
The type of bedding that occurs depends on the sediment's method of deposition, which can vary based on factors like water energy, sediment size, and environment. For example, horizontal bedding typically forms in calm water settings where fine sediments settle evenly, while cross-bedding occurs in environments with stronger currents, such as rivers or dunes, where sediments are deposited at angles. Additionally, graded bedding can form from sediment-laden flows, where coarser material settles first, followed by finer particles. Thus, the sedimentary environment significantly influences the characteristics of bedding.
What is trough cross-bedding?
A common variety of cross bedding. Generally at a relatively low angle it resembles scooped grooves. It is formed by sand dune migration (large or small scale)
