The sea can rise up.
It moves onto the land. This can happen if the land sinks. It can also happen if the ocean gets more water. This changes where we walk. Do you like the beach?
The sea can rise up.
It moves onto the land. This can happen if the land sinks. It can also happen if the ocean gets more water.
Long ago, the sea covered much of North America. It went from the Gulf to the Arctic.
Sometimes the sea goes away. This is called a regression. It can leave land behind.
During an ice age, the sea fell. It left a path between Alaska and Asia. The water levels change the world.
Sometimes the sea level rises. This is called a marine transgression.
During this event, the water moves onto higher ground. This can happen if the land sinks. It can also happen if ocean basins fill with more water.
Long ago, the sea rose across North America. It made a path called the Western Interior Seaway. This water went from the Gulf of Mexico to the Arctic Ocean. This happened because the ocean basins grew smaller.
The opposite of this is a regression. This is when the sea level falls. It leaves the old sea bottom exposed. During the Pleistocene Ice Age, the sea fell 120 meters. This left a land bridge between Alaska and Asia.
Scientists study rocks to find these changes. They look at facies, which are types of sediment. Sand is often found near the shore. Silt and mud are found in deep water. In a transgression, rocks change from sand to mud. In a regression, the pattern is the opposite. These changes help us learn about our world.
Sometimes the sea rises and moves onto higher land. This event is called a marine transgression. It happens when sea levels rise compared to the land. The shoreline moves toward higher ground and causes flooding. This can happen if the land itself sinks down. It can also happen if ocean basins fill with more water.
Many different things can cause these changes. Tectonic events like orogenies can cause them. Severe climate change, such as ice ages, also plays a part. Isostatic adjustments can happen after ice or sediment is removed. These adjustments change how the land sits. Sometimes, ocean basins simply lose their capacity to hold water. This makes the water overflow onto the land.
We can look at history to see this in action. During the Cretaceous period, seafloor spreading changed the oceans. This created a shallow Atlantic basin. It happened at the expense of a deeper Pacific basin. This reduced the total space for ocean water. Because of this, sea levels rose all over the world. The oceans even crossed the middle of North America.
This rise created the Western Interior Seaway. It stretched from the Gulf of Mexico to the Arctic Ocean. The opposite event is called a regression. This is when sea levels fall relative to the land. A regression exposes the old sea bottom. During the Pleistocene Ice Age, the sea regressed 120 meters. This exposed the Bering land bridge between Alaska and Asia.
Scientists study rocks to find these old changes. They look at facies, which are types of sediment. Sand is a coarse-grained clastic found near the shore. Fine-grained silt and mud settle in deeper, lower energy waters. In a transgression, rocks change from sandstone to marl. This change goes from the oldest to the youngest rocks. In a regression, the pattern is the exact opposite.
A marine transgression is a major geologic event. It occurs when the sea level rises relative to the land. This process causes the shoreline to move toward higher ground. As the water moves inland, it results in widespread flooding. These events change the shape of continents over long periods. They are essential for understanding how our planet's surface changes.
Several different mechanisms can drive a transgression. One cause is when the land itself begins to sink. Another cause is when ocean basins fill with more water. This can happen if the basins decrease in capacity. Tectonic events, such as orogenies, can also trigger these shifts. Severe climate change, like the onset of ice ages, plays a role. Finally, isostatic adjustments can cause changes. This happens after large amounts of ice or sediment are removed from the land.
Geologists study the opposite event, called a regression. A regression occurs when the sea level falls relative to the land. This process exposes the former sea bottom to the air. These two events are linked to the capacity of ocean basins. During the Cretaceous period, seafloor spreading changed the global ocean structure. This spreading created a relatively shallow Atlantic basin. It happened at the expense of a deeper Pacific basin. This shift reduced the total capacity of the world's ocean basins. This reduction caused a worldwide rise in sea level.
This Cretaceous sea level rise created massive new environments. The oceans transgressed completely across the central portion of North America. This created a huge body of water called the Western Interior Seaway. This seaway stretched all the way from the Gulf of Mexico to the Arctic Ocean. In contrast, the Pleistocene Ice Age caused a massive regression. During this time, so much water was removed from the oceans. The water was stored on land as year-round glaciers. The ocean regressed by as much as 120 meters. This drop exposed the Bering land bridge between Alaska and Asia.
Scientists identify these ancient events by looking at sedimentary facies. A facies is a specific type of sediment layer. Different environments require unique conditions to deposit certain sediments. For example, coarse-grained clastics like sand are common near the shore. These are found in high-energy environments where waves are strong. Fine-grained sediments, such as silt or carbonate muds, are different. These settle in deeper, lower energy waters far offshore. By looking at these layers, we can see the history of the water.
In a sedimentary column, a transgression has a specific pattern. You will see a change from nearshore facies to offshore facies. This means the oldest rocks might be sandstone, while younger rocks are marl. Marl is a type of fine-grained sediment. A regression shows the exact opposite pattern. In a regression, offshore facies change into nearshore facies. However, regressions are sometimes harder to see in the rock record. This is because their upper layers are often marked by an erosional unconformity. An unconformity is a surface where rock layers are missing due to erosion.
Identifying these events in the real world can be complicated. It is not always a simple switch between two types of rock. For instance, a regression might only show a change from carbonates to shale. A transgression might only show a change from sandstone to shale. Scientists also look at lateral changes in facies across an area. In some places, an epeiric sea may have been very deep. In other areas, the water might have been much shallower. Understanding these specific details helps geologists interpret the history of the Earth.
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