Want this question answered?
Yes, conglomerate is a sedimentary rock! It's a lithified mix of clasts, generally rounded to some degree, in a finer silt or sand matrix, all formed from deposits of the weathering products of earlier, often (but not exclusively) igneous, rock. If the clasts are coarse and angular the rock is a breccia.
== == The "coarseness" of a sedimentary rock refers to the rock's textural character, and more particularly, the size of grains contained within it. Thus, a conglomerate containing pebble or cobble clasts is coarser than a sandstone containing sand grains. In the same way, a conglomerate containing boulders is coarser than a conglomerate containing pebbles. Clastic sedimentary rocks are classified using the Wentworth Scale. The coarsest elements of this scale are the Rudites. Boulder rudites are conglomeratic rocks with grains of diameter greater than 256mm. They are the coarsest element described on the Wentworth Scale. There is no upper limit to the scale of sedimentary coarseness, since the size of clast which can be preserved in a sedimentary rocks is potentially very large. 'Olistolith' is a term which describes very large clasts often derived from the sub-sea collapse of oversteepened slopes such as are found at continental margins. Sediments containing olistoliths may reasonably be described as the coarsest sedimentary rocks.
No, conglomerate is a type of sedimentary rock made up of rounded gravel-sized particles. The particles in conglomerate are typically larger than sand grains and are often well-rounded due to the transportation and deposition processes that occur before the rock forms.
Normally, sedimentary chalk and limestone would be white (or whitish or greyish). The colour of slate can range widely, even creating green, or blue slate. Conglomerate is often coloured by the clay that surrounds the stones embedded in the clay. Even white chalk could appear reddish if contaminated enough by iron sulphates, etc.
Apologies, but I do not know what unconformity you are referring to. However, I can tell you that conglomerate IS present as an unconformity in many cases due to the nature of it's formation. Conglomerate is often produced during a flash-flood, so all rock strata from the period appear interrupted by the unconformity of Conglomerate which was deposited very quickly, then after burial was cemented and lithified. My answer, therefore, is that conglomerate is common as an unconformity.
Yes, conglomerate is a sedimentary rock! It's a lithified mix of clasts, generally rounded to some degree, in a finer silt or sand matrix, all formed from deposits of the weathering products of earlier, often (but not exclusively) igneous, rock. If the clasts are coarse and angular the rock is a breccia.
Yes, conglomerate is a sedimentary rock! It's a lithified mix of clasts, generally rounded to some degree, in a finer silt or sand matrix, all formed from deposits of the weathering products of earlier, often (but not exclusively) igneous, rock. If the clasts are coarse and angular the rock is a breccia.
== == The "coarseness" of a sedimentary rock refers to the rock's textural character, and more particularly, the size of grains contained within it. Thus, a conglomerate containing pebble or cobble clasts is coarser than a sandstone containing sand grains. In the same way, a conglomerate containing boulders is coarser than a conglomerate containing pebbles. Clastic sedimentary rocks are classified using the Wentworth Scale. The coarsest elements of this scale are the Rudites. Boulder rudites are conglomeratic rocks with grains of diameter greater than 256mm. They are the coarsest element described on the Wentworth Scale. There is no upper limit to the scale of sedimentary coarseness, since the size of clast which can be preserved in a sedimentary rocks is potentially very large. 'Olistolith' is a term which describes very large clasts often derived from the sub-sea collapse of oversteepened slopes such as are found at continental margins. Sediments containing olistoliths may reasonably be described as the coarsest sedimentary rocks.
No, conglomerate is a type of sedimentary rock made up of rounded gravel-sized particles. The particles in conglomerate are typically larger than sand grains and are often well-rounded due to the transportation and deposition processes that occur before the rock forms.
A sedimentary rock, such as sandstone (quartz mineral grains eroded, transported and set in a fine matrix of mud) or a conglomerate formed in a high energy environment such as a beach of fast-flowing river bed, containing large pebbles set in a fine to medium matrix of sand and mud grains.
A conglomerate is a combination of two or more corporations engaged in entirely different businesses that fall under one corporate structure (a corporate group), usually involving a parent company and several (or many) subsidiaries. Often, a conglomerate is a multi-industry company. Conglomerates are often large and multinational. By this definition of conglomerate (and i think the only definition) unilever is a conglomerate
== == The "coarseness" of a sedimentary rock refers to the rock's textural character, and more particularly, the size of grains contained within it. Thus, a conglomerate containing pebble or cobble clasts is coarser than a sandstone containing sand grains. In the same way, a conglomerate containing boulders is coarser than a conglomerate containing pebbles. Clastic sedimentary rocks are classified using the Wentworth Scale. The coarsest elements of this scale are the Rudites. Boulder rudites are conglomeratic rocks with grains of diameter greater than 256mm. They are the coarsest element described on the Wentworth Scale. There is no upper limit to the scale of sedimentary coarseness, since the size of clast which can be preserved in a sedimentary rocks is potentially very large. 'Olistolith' is a term which describes very large clasts often derived from the sub-sea collapse of oversteepened slopes such as are found at continental margins. Sediments containing olistoliths may reasonably be described as the coarsest sedimentary rocks.
Limestone is is a chemically altered sedimentary rock, mostly consisting of calcium carbonate in various forms. The hardness of calcite, a common ingredient, is about 3 on the Mohs scale. A conglomerate often consists of mechanically altered sedimentary rock that has been ground into relatively small pieces while being transported and deposited as sediment by glaciers. Its Mohs hardness varies, depending on the composition of the rock which is mostly a mixture of silicates, calcite, and iron compounds.
The hardness of conglomerate varies from soft to hard. It really depends on the strength and composition of the conglomerate in question. It is often used as a filler in construction, including road construction.
not that often
Normally, sedimentary chalk and limestone would be white (or whitish or greyish). The colour of slate can range widely, even creating green, or blue slate. Conglomerate is often coloured by the clay that surrounds the stones embedded in the clay. Even white chalk could appear reddish if contaminated enough by iron sulphates, etc.
Conglomerate can found at your local supermarket in a bag marked Cheetos.answer 2 Conglomerate rock is a rock made up of pebbles and sand, with the pebbles often coming from quite different sources. Typical of a rock made from the riverside gravels.