Answer:
Attraction: It includes all those factors which attract a tourist. ... Accessibility: It is how to access or reach to that place of attraction. Ways to reach. Accomodation: Place to stay or accomodate while travelling for rest or overnight stays.
<h2><em>13 x 1760 (1 Mile = 1760 yards.) = 22880.</em></h2><h2><em></em></h2><h2><em>Hope this helps and have a nice day! o/</em></h2>
Answer:
It releases bbbles of carbon dioxide
Explanation:
Answer:
river system, sandy beach or delta, plant rich swamp
Explanation:
The upper part of the stratigraphic horizon consists of Sandstone, mudstone, dust cracks with plant fossils and most significantly the coal unit. This records is quite sufficient to factor out the surroundings of deposition and prediction of supply rock. The lowermost a part of this horizon is consists of coal layers so the environment must be swampy in nature. Mud Cracks containing fossils pf plant constitute the coal are form not inside the in-situ mode they are from in ex-situ mode that means the coal isn't the autochthonous origin however are allochthonous in origin. Plant cloth comes from a different location and deposited in this zone and people not be triumphant a good decreasing situation remains as a fossil inside the dust cracks.
Mudstone include Silt and Clay which are very excellent grain particles. This mudstone is deposited in a totally low electricity circumstance of the muddy part of the ocean. This low strength condition isn't maintained for a long term and there may be a sluggish fluctuation of surroundings and high power condition cause deposition of the sandstone. Sandstone contains a number of small cross mattress which represents a beach surroundings. As a selected region document with the mud crack it is essential to say that this unique time complements the formation of coal just beneath the subsurface because the upper component is exposed to the surface.
So those are the geological history of the Upper part of the Stratigraphic horizon
you can download the attached pdf for further understanding
Answer:
D. are places where huge amounts of felsic magma have been erupted or intruded.
Explanation:
Large igneous provincession areas of great extension, have more than 100 thousand square meters, that arose as a result of the eruption of continuous magma in short geological intervals of time. Large igneous provinces consists of an accumulation of igneous rocks and features extrusive rocks, such as delava flows and pyroclast deposits.
