rose theatre: Hamlet

yesterday we went to Shakespeares rose theatre, which much to our surprise, opened again. you can see my older post by clicking here .

ok so hamlet is the play we saw. we also went to Cliffords tower were me and abbie fought to the death (well almost).

Clumber Park

On Monday we went to Clumber Park with my sister my friend and my friends mum and brother. At Clumber Park we had a picnic and there were greylag geese and they wanted our food. There was also a young squirrel who took some of my sandwich I gave my friends brother some of my sandwich to give to the squirrel after that we went to a woodland play area and me and my friends brother blew
bubbles and saw who could blow the biggest bubble.We went on a boat that had information on like when the river is low you can see the remains of a old boat that sank.

 We went on a brige that has been wrecked because some one drove back and forth and wrecked the brige there were lodes of notes saying things like we hope it is rebuilt soon and that kind of thing.
Clumber park brige is over 250 years old though

My Second STEM Session

Yesterday me and  my sister went to a STEM session. We were looking at how fossils and how bugs get stuck in Amber and I met my friend Kara and  we put a plastic bug in a half  full cup and we
put  the last three layers on .

 Metamorphic rocks are formed under the surface of the earth from the metamorphosis (change) that occurs due to intense heat and pressure (squeezing). The rocks that result from these processes often have ribbonlike layers and may have shiny crystals, formed by minerals growing slowly over time, on their surface. Examples of this rock type include gneiss and marble.

 Igneous rocks are formed when magma (molten rock deep within the earth) cools and hardens. Sometimes the magma cools inside the earth, and other times it erupts onto the surface from volcanoes (in this case, it is called lava). When lava cools very quickly, no crystals form and the rock looks shiny and glasslike. Sometimes gas bubbles are trapped in the rock during the cooling process, leaving tiny holes and spaces in the rock. Examples of this rock type include basalt and obsidian.

Sedimentary rocks are formed from particles of sand, shells, pebbles, and other fragments of material. Together, all these particles are called sediment. Gradually, the sediment accumulates in layers and over a long period of time hardens into rock. Generally, sedimentary rock is fairly soft and may break apart or crumble easily. You can often see sand, pebbles, or stones in the rock, and it is usually the only type that contains fossils. Examples of this rock type include conglomerate and limestone.