Grain size
No, magnets and sedimentary rocks have different properties. Magnets have the property of attracting certain materials like iron, while sedimentary rocks are formed through the deposition and compaction of sediment over time. Sedimentary rocks do not exhibit magnetic properties unless magnetic minerals are present in their composition.
advection
The property that best describes a rock formed from sediments is sedimentary. Sedimentary rocks are formed through the accumulation and consolidation of sediments, such as sand, silt, and clay, over time. These rocks often have distinct layers and can contain fossils.
Clastic rocks have a 'clastic texture', which means they consist of clasts. The 3D orientation of these clasts is called the fabric of the rock. Between the clasts the rock can be composed of a matrix or a cement (the latter can consist of crystals of one or more precipitated minerals). The size and form of clasts can be used to determine the velocity and direction of current in the sedimentary environment where the rock was formed; fine, calcareous mud only settles in quiet water, while gravel and larger clasts are only deposited by rapidly moving water.[10][11] The grain size of a rock is usually expressed with the Wentworth scale, though alternative scales are used sometimes. The grain size can be expressed as a diameter or a volume, and is always an average value - a rock is composed of clasts with different sizes. The statistical distribution of grain sizes is different for different rock types and is described in a property called the sorting of the rock. When all clasts are more or less of the same size, the rock is called 'well-sorted', when there is a large spread in grain size, the rock is called 'poorly sorted'
Color can be useful for identifying some sedimentary rocks, but it should not be relied upon solely as a defining characteristic. Other properties such as grain size, texture, and mineral composition are typically more reliable indicators of a sedimentary rock's identity.
the best property to find sedimentary rock is on your moms 30 acres of fat.
Make a list of the properties of each describing each property. In this way the similarities and differences will become more transparent. Asking others to complete your assignment or homework is self defeating.
forms only in a sedimentary rock
"Past indicative" is a tense, a property of verbs. In the sentence as written, however, "past indicative" is a compound noun, the name of the tense.
Out of texture and composition , it's texture.
texture as contains from ores of iron
Grain size is more important for determining the classification of clastic sedimentary rocks, such as sandstone or shale. Composition is more important for determining the classification of chemical sedimentary rocks, such as limestone or rock salt. Layering is more important for identifying the structure of sedimentary rocks, such as bedding in sandstone or shale.
No, magnets and sedimentary rocks have different properties. Magnets have the property of attracting certain materials like iron, while sedimentary rocks are formed through the deposition and compaction of sediment over time. Sedimentary rocks do not exhibit magnetic properties unless magnetic minerals are present in their composition.
advection
The verb, "was", in the sentence "He was good" is in the simple past indicative tense. A sentence as a whole is not characterized by tense, which is a property of verbs and verbals only.
The property that best describes a rock formed from sediments is sedimentary. Sedimentary rocks are formed through the accumulation and consolidation of sediments, such as sand, silt, and clay, over time. These rocks often have distinct layers and can contain fossils.
Clastic rocks have a 'clastic texture', which means they consist of clasts. The 3D orientation of these clasts is called the fabric of the rock. Between the clasts the rock can be composed of a matrix or a cement (the latter can consist of crystals of one or more precipitated minerals). The size and form of clasts can be used to determine the velocity and direction of current in the sedimentary environment where the rock was formed; fine, calcareous mud only settles in quiet water, while gravel and larger clasts are only deposited by rapidly moving water.[10][11] The grain size of a rock is usually expressed with the Wentworth scale, though alternative scales are used sometimes. The grain size can be expressed as a diameter or a volume, and is always an average value - a rock is composed of clasts with different sizes. The statistical distribution of grain sizes is different for different rock types and is described in a property called the sorting of the rock. When all clasts are more or less of the same size, the rock is called 'well-sorted', when there is a large spread in grain size, the rock is called 'poorly sorted'