0
What else can I help you with?
What is the age of the oldest sediments recovered by deep-ocean drilling?
The oldest sediments recovered by deep-ocean drilling are around 180 million years old. These sediments are typically found in the Pacific Ocean and provide valuable information about Earth's history and past environmental conditions.
What does Mississippi produce?
• Broiler (meat) chicken and soybeans are Mississippi's most valuable agricultural products. • Cotton is grown in the northwest part of the state, and the northeast part grows the majority of the cotton. • Cattle farms are common in all parts of Mississippi except the Mississippi Delta. • Mississippi ranks fourth nationally for the production of rice. The crop was valued at $178 million dollars in 2009.
How is Old Red Sandstone formed?
Old Red Sandstone is formed from the accumulation of sand and mud sediments, which solidify over time through compaction and cementation. These sediments were deposited in ancient river and lake environments during the Devonian period, around 419-359 million years ago. The distinctive red color of Old Red Sandstone rocks is due to the presence of iron oxide minerals in the sediments.
When did Pangea begin to break into smaller fragments?
Pagaea began to break apart about 180 million years ago during the Jurassic period.
What part of the Australian continent has spent the most time underwater over the last 600 million years?
The eastern part of the Australian continent, particularly in Queensland and New South Wales, has spent the most time underwater over the last 600 million years. This region has experienced several marine transgressions and regressions, resulting in the deposition of marine sediments and the formation of marine fossils.
What happens to the millions of sediments of the Mississippi river after a few million years?
Over millions of years, the sediments carried by the Mississippi River may undergo processes of compaction and cementation to form sedimentary rock layers. These layers could eventually be uplifted and exposed due to tectonic activity, allowing erosion to shape them into landforms like mountains or valleys. Ultimately, the sediments from the Mississippi River could become part of the Earth's geological record.
What happens to to sediments after a few million years?
no
What is the 2010 population for Mississippi?
2.951 million
What is the age of the oldest sediments recovered by deep-ocean drilling?
The oldest sediments recovered by deep-ocean drilling are around 180 million years old. These sediments are typically found in the Pacific Ocean and provide valuable information about Earth's history and past environmental conditions.
How much soybeans does Mississippi produce?
Mississippi produced 104 million bushels of soybeans in 2015 per the Mississippi Farm Bureau.
How many registered voters are in Mississippi?
one million five hundred sixty people
What will happen to sediments in a million years?
In a million years, sediments may undergo compaction and cementation to form sedimentary rock. They may also be uplifted due to tectonic forces and weathered into smaller particles. Overall, the sedimentary cycle will continue as new sediments are deposited on top of older ones over time.
Is Mississippi in Detroit?
No. Mississippi is a state and Detroit is a city of 5 million in Michigan. And if you're asking about the Mississippi river, no, it does not flow through Detroit.
What is the population of people in Mississippi?
The population of the state of Mississippi is 2.991 million people. Mississippi joined the Union on December 10, 1817, and its capital is Jackson.
How much was the Mississippi territory sold for?
15 million dollars
What is Mississippi's population now in 2011?
2.985 million (2012).
What happens to sediments after a million years?
After a million years, sediments can undergo diagenesis, which includes compaction and cementation. This process transforms loose sediments into solid rocks like sandstone, shale, or limestone. Over time, these rocks may be uplifted and exposed at the Earth's surface by tectonic forces.
