Till.
Glacial drift is the term for all sediments of glacier origin.
The term that refers to sediment deposited by glacier ice is "glacial till." This material is typically a mixture of various sizes of particles, ranging from clay to boulders, and is formed as glaciers advance and retreat. Glacial till is unsorted and unstratified, contrasting with sediment deposited by water, which tends to be sorted by size.
The unsorted rocky debris left behind by a melting glacier is called glacial till. It is composed of a mixture of different sizes and types of rocks, deposited as the glacier retreats and melts, creating a diverse and unsorted collection of sediments.
The term "two sediments together" typically refers to the combination or layering of different types of sedimentary materials, such as sand, silt, clay, or gravel. When these sediments are deposited in a specific environment, they can interact and form composite layers that provide insights into the geological history of an area. This combination can influence soil composition, drainage, and ecosystem development. Understanding how these sediments interact is crucial for fields like geology, archaeology, and environmental science.
Roche moutonnee: An Alpine term for a rock knob with one smooth side and one steep side, produced by glacial plucking. They are named "fleecy rocks" in French because they often look like a field of giant stone sheep. Roche moutonnee formations are sometimes called "sheepbacks" in English.
Glacial drift is the term for all sediments of glacier origin.
An annually deposited sedimentary layer is called a varve. Originally the word referred only to those annual layers of sediment deposited in a lake by glaciers, but now the more general use is accepted. Another term used in the literature is "annually laminated."
Delta
The term that refers to sediment deposited by glacier ice is "glacial till." This material is typically a mixture of various sizes of particles, ranging from clay to boulders, and is formed as glaciers advance and retreat. Glacial till is unsorted and unstratified, contrasting with sediment deposited by water, which tends to be sorted by size.
The unsorted rocky debris left behind by a melting glacier is called glacial till. It is composed of a mixture of different sizes and types of rocks, deposited as the glacier retreats and melts, creating a diverse and unsorted collection of sediments.
Sedimentation.
Moraines are composed of a mixture of rocks, gravel, sand, and clay that have been transported and deposited by glaciers. They are typically unsorted and can vary in size from tiny particles to large boulders.
Moraine is the term used to describe the deposit of loose material left behind by a glacier as it moves. This material can range from boulders to fine sediments and is typically found at the edges or terminus of a glacier. Moraines can help geologists understand the past movement and extent of glaciers.
Sediment is often deposited as the tide rises and falls. As the incoming and outgoing water crosses the beach or banks, sediments are deposited.
The term "two sediments together" typically refers to the combination or layering of different types of sedimentary materials, such as sand, silt, clay, or gravel. When these sediments are deposited in a specific environment, they can interact and form composite layers that provide insights into the geological history of an area. This combination can influence soil composition, drainage, and ecosystem development. Understanding how these sediments interact is crucial for fields like geology, archaeology, and environmental science.
Roche moutonnee: An Alpine term for a rock knob with one smooth side and one steep side, produced by glacial plucking. They are named "fleecy rocks" in French because they often look like a field of giant stone sheep. Roche moutonnee formations are sometimes called "sheepbacks" in English.
Glacier