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∙ 13y ago363 million years ago.
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∙ 13y agoHorsetails and similar plants, known as fern allies, were dominant during the Carboniferous period around 300 million years ago. They were widespread and played a significant role in shaping ancient ecosystems, contributing to the formation of coal deposits.
During the Pennsylvanian period, the Earth's surface was characterized by vast swampy areas filled with lush vegetation, including ferns, trees, and giant horsetails. These swamps eventually led to the formation of coal deposits that are still mined today. The climate was warm and humid, with shallow seas covering some areas.
Bushfires are not considered geological events, as they are primarily driven by weather conditions and human activities rather than geological processes. However, the presence of certain geological factors such as dry vegetation, topography, and climate can influence the frequency and intensity of bushfires in a particular region.
The summit area of a plateau is the highest point or points of elevation on the flat, raised landform. This area typically offers expansive views of the surrounding landscape and may include unique geological features or vegetation.
Slopes are categorized in groups called primary slopes and secondary slopes. Primary slopes promote relief while secondary slopes decrease relief. Moist areas are great for the progression of vegetation and soil.
Green vegetation covering the ground is commonly referred to as vegetation, plant cover, or simply greenery.
Hadrosaurs were able to eat tough vegetation because of the adaptations that allowed them to chew. Plants they ate may have included conifers, cycads, ferns, horsetails, and early grasses.
David J. Cantrill has written: 'The vegetation of Antarctica through geological time' -- subject(s): Plants, Evolution, SCIENCE / Paleontology, Paleontology, Paleobotany, Paleoecology, Geological time, Fossil Plants
Yes, all of them! The present one is the Holocene. The Earth's entire geological history has given us the continents, mountains and oceans we see now, mineral deposits, building-stones, vegetation types, and so on.
distinctive physical characteristics such as landforms, vegetation types, climate, and geological features. These elements combine to create unique landscapes that can be differentiated from one another.
Stegosaurus was an herbivore, or plant eater. They probably ate mosses, ferns, horsetails, cycads and conifers. A study of the bite force and teeth of Stegosaurus suggests that they couldn't bite through sticks that were more than 1.2 centimeters thick, so they would have needed to eat very tender vegetation.
Stegosaurus spent much of its time foraging for edible plants. They probably ate mosses, ferns, horsetails, cycads and conifers, but they could only reach plants within three feet of the forest floor, unless they were capable of rearing on their hind legs to reach vegetation high up in the trees.
Stegosaurus was an herbivore, or plant eater. They probably ate mosses, ferns, horsetails, cycads and conifers. A study of the bite force and teeth of Stegosaurus suggests that they couldn't bite through sticks that were more than 1.2 centimeters thick, so they would have needed to eat very tender vegetation.
Stegosaurus was an herbivore, or plant eater. They probably ate mosses, ferns, horsetails, cycads and conifers. A study of the bite force and teeth of Stegosaurus suggests that they couldn't bite through sticks that were more than 1.2 centimeters thick, so they would have needed to eat very tender vegetation.
Bushfires are not considered geological events, as they are primarily driven by weather conditions and human activities rather than geological processes. However, the presence of certain geological factors such as dry vegetation, topography, and climate can influence the frequency and intensity of bushfires in a particular region.
During the Pennsylvanian period, the Earth's surface was characterized by vast swampy areas filled with lush vegetation, including ferns, trees, and giant horsetails. These swamps eventually led to the formation of coal deposits that are still mined today. The climate was warm and humid, with shallow seas covering some areas.
Stegosaurus was an herbivore, or plant eater. They probably ate mosses, ferns, horsetails, cycads and conifers. A study of the bite force and teeth of Stegosaurus suggests that they couldn't bite through sticks that were more than 1.2 centimeters thick, so they would have needed to eat very tender vegetation.
A plain is a large, flat expanse of land characterized by low vegetation, relatively level topography, and few geological features. Plains can be found on every continent and are typically used for agriculture and grazing.